Earth Resources; Reserves and resources; Nonrenewable Mineral Resources ; What are industrial minerals?; Why are industrial minerals so important?; Geology of Industrial Minerals Deposits; Classification of industrial minerals; Factors important in evaluating an industrial minerals deposit; Selected industrial rocks and minerals
This document discusses metamorphic and metamorphosed ore deposits. It explains that metamorphic ore deposits form through the isochemical metamorphic re-equilibration and recrystallization of pre-existing materials. Contact metamorphism near magmatic bodies causes changes to fabric, mineralogy, and chemistry through processes like dewatering. Regional metamorphism can reach temperatures of 1100°C and pressures of 30 kbar, driving off volatiles and causing grain coarsening and foliation. Metamorphic fluids liberate economically valuable metals and elements and can form ore deposits as they circulate through metamorphosing rock.
This document discusses diagenetic ore deposits that form from fluids expelled during sediment compaction and lithification. It provides examples of deposit types formed this way, including the European Copper Shale and Mississippi Valley Type lead-zinc deposits. The core concept is that sediments contain large volumes of connate/formation waters that are expelled during diagenesis, becoming enriched in metals. When these hot, high-pressure fluids pass through permeability traps in the basinal sediments, they can precipitate ore minerals and form economic deposits. Microbes and geochemical conditions also influence metal mobility and deposition during this process.
Geological criteria for ore prospectingPramoda Raj
This document outlines various geological criteria that can be used for ore prospecting, including stratigraphic, lithological, structural, magmatogenic, metamorphogenic, geomorphological, paleogeographical, paleoclimatic, and historical criteria. Specific examples are provided for each criteria, such as coal and iron ore deposits being associated with specific stratigraphic layers, or chromite and diamond deposits found near ultrabasic rocks. The document emphasizes that geological criteria provide indirect methods for locating ore deposits and should be used to guide prospecting efforts.
This document discusses genetic classification of ore deposits. It notes that while various geological aspects like metals, orebody form, environment, and tectonic setting are used to classify deposits, a stringent genetic classification is difficult for two reasons. First, many deposits represent complex combinations of well-defined end members like volcanic, intrusive, sedimentary and diagenetic processes. Second, the origin of deposits like Kuroko and high-grade BIF-haematite seems to involve multiple geological processes interacting, like marine life proliferation and saline brine passage. The document recommends reading a specific review article for further detailed classification information.
Abu Dabbab and Nuweibi deposits (tantalum-tin-feldspar), Feasibility study upgrade,Gippsland,tantalum-tin project located on the western shore of the Red Sea;Abu Dabbab and Nuweibi tantalum-tin-feldspar deposits having a combined resource of 138 million tonnes;The Company’s Abu Dabbab and Nuweibi tantalum deposits will be developed to establish Gippsland as a leading global tantalum producer for several decades
Ever wondered what makes the industrial minerals market tick? Just how does it differ from the metal minerals market? Thinking of investing in industrial minerals?
Industrial Minerals Basics: Executive Primer is a concise overview presentation for a quick but informed assessment of key elements of the industrial minerals business. Ideal as an introduction for first timers, or as a refresher for those already in the business.
Contents:
What are industrial minerals?
Why are they so important?
How is the market structured?
How is the market driven?
Summary
Which key factors influence success?
Please contact me with any questions or comments: mike@modriscollminerals.com
This document provides information on igneous petrology and the classification of igneous rocks. It discusses different classification systems including genetic, textural, chemical, and mineralogical classifications. It also describes techniques for chemical analysis of rocks and key concepts in igneous petrology such as saturation, variation diagrams, and the use of major and trace elements to understand rock origins.
Earth Resources; Reserves and resources; Nonrenewable Mineral Resources ; What are industrial minerals?; Why are industrial minerals so important?; Geology of Industrial Minerals Deposits; Classification of industrial minerals; Factors important in evaluating an industrial minerals deposit; Selected industrial rocks and minerals
This document discusses metamorphic and metamorphosed ore deposits. It explains that metamorphic ore deposits form through the isochemical metamorphic re-equilibration and recrystallization of pre-existing materials. Contact metamorphism near magmatic bodies causes changes to fabric, mineralogy, and chemistry through processes like dewatering. Regional metamorphism can reach temperatures of 1100°C and pressures of 30 kbar, driving off volatiles and causing grain coarsening and foliation. Metamorphic fluids liberate economically valuable metals and elements and can form ore deposits as they circulate through metamorphosing rock.
This document discusses diagenetic ore deposits that form from fluids expelled during sediment compaction and lithification. It provides examples of deposit types formed this way, including the European Copper Shale and Mississippi Valley Type lead-zinc deposits. The core concept is that sediments contain large volumes of connate/formation waters that are expelled during diagenesis, becoming enriched in metals. When these hot, high-pressure fluids pass through permeability traps in the basinal sediments, they can precipitate ore minerals and form economic deposits. Microbes and geochemical conditions also influence metal mobility and deposition during this process.
Geological criteria for ore prospectingPramoda Raj
This document outlines various geological criteria that can be used for ore prospecting, including stratigraphic, lithological, structural, magmatogenic, metamorphogenic, geomorphological, paleogeographical, paleoclimatic, and historical criteria. Specific examples are provided for each criteria, such as coal and iron ore deposits being associated with specific stratigraphic layers, or chromite and diamond deposits found near ultrabasic rocks. The document emphasizes that geological criteria provide indirect methods for locating ore deposits and should be used to guide prospecting efforts.
This document discusses genetic classification of ore deposits. It notes that while various geological aspects like metals, orebody form, environment, and tectonic setting are used to classify deposits, a stringent genetic classification is difficult for two reasons. First, many deposits represent complex combinations of well-defined end members like volcanic, intrusive, sedimentary and diagenetic processes. Second, the origin of deposits like Kuroko and high-grade BIF-haematite seems to involve multiple geological processes interacting, like marine life proliferation and saline brine passage. The document recommends reading a specific review article for further detailed classification information.
Abu Dabbab and Nuweibi deposits (tantalum-tin-feldspar), Feasibility study upgrade,Gippsland,tantalum-tin project located on the western shore of the Red Sea;Abu Dabbab and Nuweibi tantalum-tin-feldspar deposits having a combined resource of 138 million tonnes;The Company’s Abu Dabbab and Nuweibi tantalum deposits will be developed to establish Gippsland as a leading global tantalum producer for several decades
Ever wondered what makes the industrial minerals market tick? Just how does it differ from the metal minerals market? Thinking of investing in industrial minerals?
Industrial Minerals Basics: Executive Primer is a concise overview presentation for a quick but informed assessment of key elements of the industrial minerals business. Ideal as an introduction for first timers, or as a refresher for those already in the business.
Contents:
What are industrial minerals?
Why are they so important?
How is the market structured?
How is the market driven?
Summary
Which key factors influence success?
Please contact me with any questions or comments: mike@modriscollminerals.com
This document provides information on igneous petrology and the classification of igneous rocks. It discusses different classification systems including genetic, textural, chemical, and mineralogical classifications. It also describes techniques for chemical analysis of rocks and key concepts in igneous petrology such as saturation, variation diagrams, and the use of major and trace elements to understand rock origins.
Gives a short discussion about ore, terms like precipitation, hydothermal solution and the four different types of hydrothermal ore deposits including vein type, disseminated, massive sulfide, and stratabound deposits. Hope you'll enjoy and understand it!
1. Fluid inclusion studies were conducted on samples from 10 wells in the Irish Porcupine Basin to determine the chronology of aqueous and oil-bearing fluids during basin evolution.
2. Three types of fluid inclusions were identified: low-salinity aqueous inclusions; monophase aqueous inclusions; and two-phase oil-bearing inclusions.
3. Oil-bearing inclusions observed in Jurassic sandstone cements and grains indicate trapping of heavier, less mature oil early during cementation and later ingress of lighter, more mature oil.
This document discusses hydrothermal fluids and hydrothermal ore deposits. It begins by describing the different types of fluids found in the Earth's crust, including sea water, meteoric water, connate water, metamorphic water, and mixtures. For hydrothermal deposits to form, these fluids need to circulate through the crust to dissolve and transport metals. Common hydrothermal deposit types include veins and cavity fillings. Veins can be fissure, ladder, or gash veins and cavity fillings include saddle reefs. Metal solubility in hydrothermal fluids is controlled by factors like temperature, pH, and ligand complexes. Precipitation occurs when solubility decreases, such as due to changes in fluid composition or physical properties like
Biogeochemical anomalies occur where vegetation contains abnormally high concentrations of metals. Different plant species take up different amounts of inorganic materials from the soil based on factors like their root depth and water source. Plants with deep roots directly over an ore deposit can show biogeochemical anomalies from taking up mobile elements in soil solutions. Biogeochemical surveys first determine the optimal plant species, plant part, and elements to sample through an orientation survey. They then involve systematically collecting and analyzing plant samples according to a grid or vegetation distribution to identify anomalies.
This document discusses supergene ore formation systems resulting from chemical weathering of rocks. Supergene deposits form through two main processes - enrichment of valuable components in a residual left after dissolution/transport of other materials, or dissolution/transport/reprecipitation of valuable components. Key points: Bauxite, lateritic nickel/iron/gold/manganese deposits form through residual enrichment. Conditions like climate, vegetation influence weathering rates and supergene processes. Laterite profiles can be over 100m thick with vertical chemical zonation. Residual/eluvial placers concentrate weathering-resistant minerals.
Models and exploration methods for major gold deposit typesMYO AUNG Myanmar
Models and Exploration Methods for Major Gold Deposit Types
Robert, F.[1], Brommecker, R.[1] Bourne, B. T.[2]
, Dobak, P. J.3], McEwan, C. .J.[4],Rowe, R. R.[2], Zhou, X.
[1]
_________________________ 1. Barrick Gold Corporation, Toronto, ON
, Canada
2. Barrick Gold of Australia Ltd., Perth, WA, Australia 3. Barrick Gold Exploration Inc., Elko, NV, U.S.A 4. Compania Minera Barrick Chile Ltda., Providencia, Santiago, Chile
ABSTRACT
Gold occurs as primary commodity in a wide range of gold deposit types and settings. In the last decade, significant progress has been made in the classification, definition and understanding of the main gold deposit types. Three main clans of deposits are now broadly
defined, each including a range of specific de
posit types with common characteristics and tectonic settings. The orogenic clan has
been introduced to include vein
-
type deposits formed during crustal shortening of their host greenstone, BIF or clastic sedimentary
rock sequences. Deposits of the new red
uced intrusion-
related clan share an Au
- Bi-
Te
-
As metal signature and an association with
moderately reduced equigranular post
-
orogenic granitic intrusions. Oxidized intrusion-related deposits, including porphyry, skarn,and high-
sulfidation epithermal depo sits, are associated with high-
level, oxidized porphyry stocks in magmatic arcs. Other important deposit types include Carlin, low sulfidation pithermal, Au,rich VMS and Witwatersrand deposits. The key geology features of the ore- forming environments and the key geologic manifestations of the different deposit types form the footprints of ore systems that are targeted in exploration programs. Important progress has been made in our ability to integrate, process, and visualize increasingly complex datasets
in 2D GIS and 3D platforms. For gold exploration, important geophysical advances include airborne gravity, routine 3D inversions of potential field data, and 3D modeling of electrical data. Improved satellite -, airborne- and field-based
infrared spectroscopy has significantly improved alteration mapping around gold systems, extending the dimensions of the footprints and enhancing vectoring capabilities. Conventional geochemistry remains very important to gold exploration, while promising new techniques are
being tested. Selection of the appropriate exploration methods must be dictated by the characteristics of the targeted model, its geologic setting, and the surficial environment. Both greenfield and brownfield exploration contributed to the discovery of ma jor gold deposits (>2.5 moz Au) in the last decade but the discovery rates have declined significantly. Geologists are now better equipped than ever to face this difficult challenge, but geological understanding and quality field work were important discov ery factors and must remain the key underpinnings of exploration programs
Gold is a transitional metal. In its purest form have reddish yellow color, soft, malleable, and ductile metal.
Atomic number : 79
Atomic mass : 196.9 u
Density : 19.32 g/cm3
Melting point : 1,064 °C
Boiling point : 2,700 °C
Founded in different form associated with different rock type in different tectonic setting.
Discovered from earlier time and used for multi purposes.
Formation of gold
The saying among prospectors that "gold is where you find it" suggests its occurrence is unpredictable, but there is some certain geological environments for the formation.
Because gold is very stable over a range of conditions, it is very widespread in the earth’s crust.
Gold dissolved in warm to hot salty water, the fluids are generated in huge volumes deep in the Earth’s crust as water-bearing minerals dehydrate during metamorphism.
Any gold present in the rocks being heated and squeezed is sweated out and goes into solution as complex ions.
In this form, dissolved gold, along with other elements such as silicon, iron and sulphur, migrates wherever fractures in the rocks allow the fluids to pass.
The direction is generally upwards, to cooler regions at lower pressures nearer the Earth’s surface.
Gold eventually becomes insoluble and begins to crystallize, most often enveloped by quartz.
The association of gold and quartz vein forms one of the most common types of "primary gold deposits".
India
In India, gold mineralization of economic importance is mainly restricted to Archean greenstone terranes of the Dharwar Craton (DC).
The eastern block of the DC has a high favorability for hosting major gold deposits such as Kolar, Hutti, and Ramagiri, whereas the western block hosts only a few smaller deposits such as Gadag, Ajjahanahalli, and Kempinkote.
Gold also discoverrd by GSI in the Singbhum Craton, Aravalli Craton, Bastar Craton and Southern Granulite Terrain (SGT).
India is the second-largest consumer of gold after China.
India currently holds about 558 tones of gold, representing 6.6% of its reserves, (World Gold Council, October 2016).
Kolar Gold Field, Hutti Gold Field and Ramgiri Gold Field are the most important gold fields.
Gold Demand and Use
The largest source of demand is the jewelry industry Gold’s workability, unique beauty, and universal appeal make this rare precious metal the favorite of jewelers all over the world.
Besides jewelry, gold has many applications in a variety of industries including aerospace, medicine, dentistry, and electronics for the manufacture of computers, telephones, televisions...
The third source of gold demand is governments and central banks that buy gold to increase their official reserves.
Private investors there are private investors. Depending upon market circumstances, the investment component of demand can vary substantially from year to year.
The document discusses a lecture on ore deposit classification and ore reserves. It covers the Joint Ore Reserves Committee (JORC) code for classifying and reporting mineral resources and ore reserves. Key aspects of the code are transparency, materiality, and competence. It also discusses definitions of mineral resources, probable and proved ore reserves. The lecture covers different types of ore deposits based on their geologic settings, including stratiform, discordant, and concordant deposits in various host rock types. Terminology related to ore deposits and textures seen in hand samples are also defined. Theories of ore genesis involving internal magmatic and hydrothermal processes as well as surface processes are outlined.
This document discusses the process of prospecting for and proving a mineral deposit. It begins by defining prospecting and mining. Prospecting aims to initially find deposits, while proving works to establish the deposit's parameters, quality, and reserves. The process involves three stages - prospecting, exploration, and proving. Exploration methods discussed include remote sensing, mapping, geophysics, geochemistry, and drilling. Proving then further defines the deposit through deeper drilling, sampling, determining reserves and establishing a mining plan. Developing accurate ore deposit models is also an important part of effectively exploring for and proving deposits.
Mineral exploration is the process of finding ore deposits to mine through organized prospecting. The most crucial part is selecting suitable areas based on geology and terrain to make exploration easy, cheap, and quick. Common exploration methods include geophysics using physical measurements, remote sensing using aerial technologies like satellites, and geochemical methods to identify anomalies within mineral deposit areas. The ultimate goal of exploration is the extraction and profitable sale of identified minerals, though there are risks from changing prices and weather conditions that could delay revenue generation.
Mechanical concentration forms placer deposits by separating heavy minerals from light ones using gravity and moving fluids like water or air. Placer deposits can form in various environments including along hill slopes (eluvial placers), in streams (alluvial placers), on beaches, and from wind (eolian placers). Key factors that influence concentration include differences in mineral density, size, shape, and the velocity of the moving fluid. Common minerals found in placer deposits include gold, platinum, tin, magnetite, and chromite due to their high density and resistance to weathering.
Uranium Deposits
Uranium is a very dense metal which can be used as an abundant source of concentrated energy. It occurs in most rocks in concentrations of 2 to 4 parts per million and is as common in the earth's crust as tin, tungsten and molybdenum.
.
There are three main types of uranium deposits including 1. unconformity-type deposits, 2. paleoplacer deposits and 3. sandstone-type (roll front) deposits (Figure 1). Sandstone-type deposits are abundant in sedimentary rocks of the Colorado Plateau and found on the Navajo Nation. This type of uranium deposit is easier and cheaper to mine than the other types because the uranium is found near the surface of the Earth. These deposits formed when oxidized groundwater that had leached uranium from surface rocks flowed down into aquifers, where it was reduced to precipitate uraninite, the primary ore mineral of uranium. In some deposits, like those found on the Navajo Nation, reduction took place along curved zones know as roll-fronts, which represent the transition from oxidized to reduced conditions in the aquifer.
Porphyry copper deposits form near shallow porphyritic intrusions where hydrothermal fluids interact with the intrusion and surface waters. Characteristic alteration minerals like chlorite, epidote, clays and micas form from the reaction of hydrothermal solutions with igneous rock silicates. Primary sulfide minerals like chalcopyrite and bornite near the intrusion are oxidized in the supergene zone to form secondary copper minerals and oxides, leaving a gossan at the surface. In contrast, epithermal deposits form at even shallower depths dominated by surface waters and produce a variety of ore minerals including gold, silver, lead and zinc.
The document discusses various atomic minerals found in India including uranium, thorium, beryllium, and lithium. It provides details on the largest reserves of each mineral by state in India and largest producing countries globally. The major uses of each mineral are also summarized, with uranium and thorium being primarily used for nuclear energy production, beryllium for alloys, and lithium for batteries.
Sampling is used to estimate grades and contents of materials in a deposit. The objective is to do this in an unbiased, precise manner. There are different sampling methods depending on the type of deposit, including core drilling, channel sampling, and trench sampling. Samples are analyzed to determine their physical and chemical characteristics, which provides information about the deposit for resource evaluation and process design.
This document discusses coal rank, grade, and type. It provides definitions and classifications for these coal properties.
Coal rank refers to the degree of coalification or thermal maturation of coal, ranging from lignite to anthracite. Coal grade is based on purity and ash content. Coal type is distinguished by the type of plant materials that formed the coal. These properties are independent but can vary spatially. Coal is first classified by rank to determine its utilization. Rank is determined through parameters like carbon content, energy value, and maceral composition that change with the coalification process. Coal plies form a basis for sampling and correlation within a coal seam based on variations in lithotype or partings.
This document provides an outline for a lecture series on mining geology. It introduces key concepts related to mining, including definitions of mining, minerals, and ore deposits. It discusses various types of ore deposits and characteristics that determine their economic viability, such as grade, shape, depth, and stability. The document also lists topics that will be covered in each lecture, including ore mineralogy, the mining cycle, resource classification, mining methods, processing, waste management, and environmental issues. The series aims to give students a non-technical overview of the mining and mineral extraction process.
The document provides a field report from a 4-day trip to the Salt Range in Pakistan. It includes observations and descriptions of the local geology, stratigraphy, and paleontology. Chapters discuss the tectonics of the area and examine various road sections and sites in detail. Lithologies, fossils, and sedimentary features of 16 different formations are described. The field trip enhanced the students' understanding of the local geology and helped them learn skills like determining strike and dip of rock units.
Information about these fluids is an invaluable aid in mineral exploration.
Conventional academic methods of analysing fluid inclusions are too slow and tedious to be of practical application in typical mineral exploration activities.
However, the academic data from numerous studies does show that CO2 is an exceptionally important indicator when exploring for most types of gold deposit.
Because the baro-acoustic decrepitation method is a rapid and reliable method to measure CO2 contents in fluids, it can be used to study a spatial array of data and it is an invaluable and practical exploration method.
Measurements of temperatures of fluid inclusions does not usually help in mineral exploration as hydrothermal minerals deposit over a wide temperature range and there is no specific temperature which is indicative of mineralisation. However, if temperatures are available on a large spatial array of samples, then temperature trends may be a useful exploration method to find the hottest part of the system, which is presumably the location of the best economic mineralisation. Baro-acoustic decrepitation is the most practical method to determine temperatures of the large numbers of samples required.
Salinities of fluid inclusions are of limited use in exploration and are difficult to measure. However, they can be used to recognise intrusion related hydrothermal systems.
Gives a short discussion about ore, terms like precipitation, hydothermal solution and the four different types of hydrothermal ore deposits including vein type, disseminated, massive sulfide, and stratabound deposits. Hope you'll enjoy and understand it!
1. Fluid inclusion studies were conducted on samples from 10 wells in the Irish Porcupine Basin to determine the chronology of aqueous and oil-bearing fluids during basin evolution.
2. Three types of fluid inclusions were identified: low-salinity aqueous inclusions; monophase aqueous inclusions; and two-phase oil-bearing inclusions.
3. Oil-bearing inclusions observed in Jurassic sandstone cements and grains indicate trapping of heavier, less mature oil early during cementation and later ingress of lighter, more mature oil.
This document discusses hydrothermal fluids and hydrothermal ore deposits. It begins by describing the different types of fluids found in the Earth's crust, including sea water, meteoric water, connate water, metamorphic water, and mixtures. For hydrothermal deposits to form, these fluids need to circulate through the crust to dissolve and transport metals. Common hydrothermal deposit types include veins and cavity fillings. Veins can be fissure, ladder, or gash veins and cavity fillings include saddle reefs. Metal solubility in hydrothermal fluids is controlled by factors like temperature, pH, and ligand complexes. Precipitation occurs when solubility decreases, such as due to changes in fluid composition or physical properties like
Biogeochemical anomalies occur where vegetation contains abnormally high concentrations of metals. Different plant species take up different amounts of inorganic materials from the soil based on factors like their root depth and water source. Plants with deep roots directly over an ore deposit can show biogeochemical anomalies from taking up mobile elements in soil solutions. Biogeochemical surveys first determine the optimal plant species, plant part, and elements to sample through an orientation survey. They then involve systematically collecting and analyzing plant samples according to a grid or vegetation distribution to identify anomalies.
This document discusses supergene ore formation systems resulting from chemical weathering of rocks. Supergene deposits form through two main processes - enrichment of valuable components in a residual left after dissolution/transport of other materials, or dissolution/transport/reprecipitation of valuable components. Key points: Bauxite, lateritic nickel/iron/gold/manganese deposits form through residual enrichment. Conditions like climate, vegetation influence weathering rates and supergene processes. Laterite profiles can be over 100m thick with vertical chemical zonation. Residual/eluvial placers concentrate weathering-resistant minerals.
Models and exploration methods for major gold deposit typesMYO AUNG Myanmar
Models and Exploration Methods for Major Gold Deposit Types
Robert, F.[1], Brommecker, R.[1] Bourne, B. T.[2]
, Dobak, P. J.3], McEwan, C. .J.[4],Rowe, R. R.[2], Zhou, X.
[1]
_________________________ 1. Barrick Gold Corporation, Toronto, ON
, Canada
2. Barrick Gold of Australia Ltd., Perth, WA, Australia 3. Barrick Gold Exploration Inc., Elko, NV, U.S.A 4. Compania Minera Barrick Chile Ltda., Providencia, Santiago, Chile
ABSTRACT
Gold occurs as primary commodity in a wide range of gold deposit types and settings. In the last decade, significant progress has been made in the classification, definition and understanding of the main gold deposit types. Three main clans of deposits are now broadly
defined, each including a range of specific de
posit types with common characteristics and tectonic settings. The orogenic clan has
been introduced to include vein
-
type deposits formed during crustal shortening of their host greenstone, BIF or clastic sedimentary
rock sequences. Deposits of the new red
uced intrusion-
related clan share an Au
- Bi-
Te
-
As metal signature and an association with
moderately reduced equigranular post
-
orogenic granitic intrusions. Oxidized intrusion-related deposits, including porphyry, skarn,and high-
sulfidation epithermal depo sits, are associated with high-
level, oxidized porphyry stocks in magmatic arcs. Other important deposit types include Carlin, low sulfidation pithermal, Au,rich VMS and Witwatersrand deposits. The key geology features of the ore- forming environments and the key geologic manifestations of the different deposit types form the footprints of ore systems that are targeted in exploration programs. Important progress has been made in our ability to integrate, process, and visualize increasingly complex datasets
in 2D GIS and 3D platforms. For gold exploration, important geophysical advances include airborne gravity, routine 3D inversions of potential field data, and 3D modeling of electrical data. Improved satellite -, airborne- and field-based
infrared spectroscopy has significantly improved alteration mapping around gold systems, extending the dimensions of the footprints and enhancing vectoring capabilities. Conventional geochemistry remains very important to gold exploration, while promising new techniques are
being tested. Selection of the appropriate exploration methods must be dictated by the characteristics of the targeted model, its geologic setting, and the surficial environment. Both greenfield and brownfield exploration contributed to the discovery of ma jor gold deposits (>2.5 moz Au) in the last decade but the discovery rates have declined significantly. Geologists are now better equipped than ever to face this difficult challenge, but geological understanding and quality field work were important discov ery factors and must remain the key underpinnings of exploration programs
Gold is a transitional metal. In its purest form have reddish yellow color, soft, malleable, and ductile metal.
Atomic number : 79
Atomic mass : 196.9 u
Density : 19.32 g/cm3
Melting point : 1,064 °C
Boiling point : 2,700 °C
Founded in different form associated with different rock type in different tectonic setting.
Discovered from earlier time and used for multi purposes.
Formation of gold
The saying among prospectors that "gold is where you find it" suggests its occurrence is unpredictable, but there is some certain geological environments for the formation.
Because gold is very stable over a range of conditions, it is very widespread in the earth’s crust.
Gold dissolved in warm to hot salty water, the fluids are generated in huge volumes deep in the Earth’s crust as water-bearing minerals dehydrate during metamorphism.
Any gold present in the rocks being heated and squeezed is sweated out and goes into solution as complex ions.
In this form, dissolved gold, along with other elements such as silicon, iron and sulphur, migrates wherever fractures in the rocks allow the fluids to pass.
The direction is generally upwards, to cooler regions at lower pressures nearer the Earth’s surface.
Gold eventually becomes insoluble and begins to crystallize, most often enveloped by quartz.
The association of gold and quartz vein forms one of the most common types of "primary gold deposits".
India
In India, gold mineralization of economic importance is mainly restricted to Archean greenstone terranes of the Dharwar Craton (DC).
The eastern block of the DC has a high favorability for hosting major gold deposits such as Kolar, Hutti, and Ramagiri, whereas the western block hosts only a few smaller deposits such as Gadag, Ajjahanahalli, and Kempinkote.
Gold also discoverrd by GSI in the Singbhum Craton, Aravalli Craton, Bastar Craton and Southern Granulite Terrain (SGT).
India is the second-largest consumer of gold after China.
India currently holds about 558 tones of gold, representing 6.6% of its reserves, (World Gold Council, October 2016).
Kolar Gold Field, Hutti Gold Field and Ramgiri Gold Field are the most important gold fields.
Gold Demand and Use
The largest source of demand is the jewelry industry Gold’s workability, unique beauty, and universal appeal make this rare precious metal the favorite of jewelers all over the world.
Besides jewelry, gold has many applications in a variety of industries including aerospace, medicine, dentistry, and electronics for the manufacture of computers, telephones, televisions...
The third source of gold demand is governments and central banks that buy gold to increase their official reserves.
Private investors there are private investors. Depending upon market circumstances, the investment component of demand can vary substantially from year to year.
The document discusses a lecture on ore deposit classification and ore reserves. It covers the Joint Ore Reserves Committee (JORC) code for classifying and reporting mineral resources and ore reserves. Key aspects of the code are transparency, materiality, and competence. It also discusses definitions of mineral resources, probable and proved ore reserves. The lecture covers different types of ore deposits based on their geologic settings, including stratiform, discordant, and concordant deposits in various host rock types. Terminology related to ore deposits and textures seen in hand samples are also defined. Theories of ore genesis involving internal magmatic and hydrothermal processes as well as surface processes are outlined.
This document discusses the process of prospecting for and proving a mineral deposit. It begins by defining prospecting and mining. Prospecting aims to initially find deposits, while proving works to establish the deposit's parameters, quality, and reserves. The process involves three stages - prospecting, exploration, and proving. Exploration methods discussed include remote sensing, mapping, geophysics, geochemistry, and drilling. Proving then further defines the deposit through deeper drilling, sampling, determining reserves and establishing a mining plan. Developing accurate ore deposit models is also an important part of effectively exploring for and proving deposits.
Mineral exploration is the process of finding ore deposits to mine through organized prospecting. The most crucial part is selecting suitable areas based on geology and terrain to make exploration easy, cheap, and quick. Common exploration methods include geophysics using physical measurements, remote sensing using aerial technologies like satellites, and geochemical methods to identify anomalies within mineral deposit areas. The ultimate goal of exploration is the extraction and profitable sale of identified minerals, though there are risks from changing prices and weather conditions that could delay revenue generation.
Mechanical concentration forms placer deposits by separating heavy minerals from light ones using gravity and moving fluids like water or air. Placer deposits can form in various environments including along hill slopes (eluvial placers), in streams (alluvial placers), on beaches, and from wind (eolian placers). Key factors that influence concentration include differences in mineral density, size, shape, and the velocity of the moving fluid. Common minerals found in placer deposits include gold, platinum, tin, magnetite, and chromite due to their high density and resistance to weathering.
Uranium Deposits
Uranium is a very dense metal which can be used as an abundant source of concentrated energy. It occurs in most rocks in concentrations of 2 to 4 parts per million and is as common in the earth's crust as tin, tungsten and molybdenum.
.
There are three main types of uranium deposits including 1. unconformity-type deposits, 2. paleoplacer deposits and 3. sandstone-type (roll front) deposits (Figure 1). Sandstone-type deposits are abundant in sedimentary rocks of the Colorado Plateau and found on the Navajo Nation. This type of uranium deposit is easier and cheaper to mine than the other types because the uranium is found near the surface of the Earth. These deposits formed when oxidized groundwater that had leached uranium from surface rocks flowed down into aquifers, where it was reduced to precipitate uraninite, the primary ore mineral of uranium. In some deposits, like those found on the Navajo Nation, reduction took place along curved zones know as roll-fronts, which represent the transition from oxidized to reduced conditions in the aquifer.
Porphyry copper deposits form near shallow porphyritic intrusions where hydrothermal fluids interact with the intrusion and surface waters. Characteristic alteration minerals like chlorite, epidote, clays and micas form from the reaction of hydrothermal solutions with igneous rock silicates. Primary sulfide minerals like chalcopyrite and bornite near the intrusion are oxidized in the supergene zone to form secondary copper minerals and oxides, leaving a gossan at the surface. In contrast, epithermal deposits form at even shallower depths dominated by surface waters and produce a variety of ore minerals including gold, silver, lead and zinc.
The document discusses various atomic minerals found in India including uranium, thorium, beryllium, and lithium. It provides details on the largest reserves of each mineral by state in India and largest producing countries globally. The major uses of each mineral are also summarized, with uranium and thorium being primarily used for nuclear energy production, beryllium for alloys, and lithium for batteries.
Sampling is used to estimate grades and contents of materials in a deposit. The objective is to do this in an unbiased, precise manner. There are different sampling methods depending on the type of deposit, including core drilling, channel sampling, and trench sampling. Samples are analyzed to determine their physical and chemical characteristics, which provides information about the deposit for resource evaluation and process design.
This document discusses coal rank, grade, and type. It provides definitions and classifications for these coal properties.
Coal rank refers to the degree of coalification or thermal maturation of coal, ranging from lignite to anthracite. Coal grade is based on purity and ash content. Coal type is distinguished by the type of plant materials that formed the coal. These properties are independent but can vary spatially. Coal is first classified by rank to determine its utilization. Rank is determined through parameters like carbon content, energy value, and maceral composition that change with the coalification process. Coal plies form a basis for sampling and correlation within a coal seam based on variations in lithotype or partings.
This document provides an outline for a lecture series on mining geology. It introduces key concepts related to mining, including definitions of mining, minerals, and ore deposits. It discusses various types of ore deposits and characteristics that determine their economic viability, such as grade, shape, depth, and stability. The document also lists topics that will be covered in each lecture, including ore mineralogy, the mining cycle, resource classification, mining methods, processing, waste management, and environmental issues. The series aims to give students a non-technical overview of the mining and mineral extraction process.
The document provides a field report from a 4-day trip to the Salt Range in Pakistan. It includes observations and descriptions of the local geology, stratigraphy, and paleontology. Chapters discuss the tectonics of the area and examine various road sections and sites in detail. Lithologies, fossils, and sedimentary features of 16 different formations are described. The field trip enhanced the students' understanding of the local geology and helped them learn skills like determining strike and dip of rock units.
Information about these fluids is an invaluable aid in mineral exploration.
Conventional academic methods of analysing fluid inclusions are too slow and tedious to be of practical application in typical mineral exploration activities.
However, the academic data from numerous studies does show that CO2 is an exceptionally important indicator when exploring for most types of gold deposit.
Because the baro-acoustic decrepitation method is a rapid and reliable method to measure CO2 contents in fluids, it can be used to study a spatial array of data and it is an invaluable and practical exploration method.
Measurements of temperatures of fluid inclusions does not usually help in mineral exploration as hydrothermal minerals deposit over a wide temperature range and there is no specific temperature which is indicative of mineralisation. However, if temperatures are available on a large spatial array of samples, then temperature trends may be a useful exploration method to find the hottest part of the system, which is presumably the location of the best economic mineralisation. Baro-acoustic decrepitation is the most practical method to determine temperatures of the large numbers of samples required.
Salinities of fluid inclusions are of limited use in exploration and are difficult to measure. However, they can be used to recognise intrusion related hydrothermal systems.
Choice of mining and processing methods; Choice of mining method; What determines the type of mining?; Types of Mining; Processes and Considerations; Surface and underground mining: what’s the difference?
Egyptian Phosphate Ore Deposits; Red Sea Coast Phosphate Deposits; Nile Valley Phosphate Deposits; New Valley Geological Setting of Egyptian Phosphate; Geology of the Main Phosphate Regions; Egyptian Phosphate Ore Deposits:; Red Sea Coast Phosphate Deposits; Nile Valley Phosphate Deposits; New Valley Phosphate Deposits; Abu Tartur Ore Phosphate; Dakhla Phosphate; Common Characters of the Egyptian Phosphorites; Characteristics of the phosphate producing facies area; Phosphate Microfacies; Mineralogical composition ; Geochemistry ; Phosphate Reserves and Production
MINERAL RESOURCE AND RESERVE DECLARATIONS AND ASSET MANAGEMENT; Resource Evaluation; Mineral Resource Asset Management; Inferred Mineral Resources; Indicated Mineral Resources; Measured Mineral Resources; Mineral reserves; Reserve definition; Feasibility study; GEOLOGIC CONDITIONS AND CHARACTERISTIC OF ORE DEPOSITS; MINE GEOLOGY RESPONSIBILITIES; Geological Database Configuration; Ore Control Process
MINE LIFE CYCLE; LIFE CYCLE OF DEPOSITS; LIFE-CYCLE OF A MINE PROJECT; STAGES IN THE LIFE CYCLE OF A MINE PROJECT; Prospecting; Exploration ; 3D modeling software's for mining sectors; Mineral Resource; Mineral Reserve; Development; Exploitation ; MINE PLANNING CYCLE ; Reclamation; ENVIRONMENTAL IMPACTS OF NONRENEWABLE MINERAL RESOURCES; SOURCES OF METAL POLLUTION; Harmful Environmental Effects of Mining; Persistent, Bio-accumulative and Toxi (PBT ); Lead; Mercury; Cadmium; Arsenic
IRON ORE DEPOSITS IN EGYPT ; EGYPTIAN IRON ORE DEPOSITS; Iron ore deposit of sedimentary nature; Sinai: Gabal Halal iron ore deposit; Western Desert:; Aswan iron Ore Deposits; Bahariya iron Ore Deposits; The Banded Iron ore deposits (BIFs), Geologic Setting BIFs, General Characteristics of the Egyptian Banded Iron Ores; Are the Egyptian Banded Iron Ores Unique?; Genesis of Egyptian Banded Iron Formation
This document discusses processing sand and silica sand into other materials. It begins by outlining examples of mineral processing including sand, silica sand, and heavy mineral sand. For processing sand and silica sand, it describes extracting, washing, classifying, and removing impurities from the sand through steps like screening, attrition scrubbing, hydrocyclones, and magnetic separation. The sand can then be further processed into silicon, silicon carbide, and silicone through reducing silica to ferrosilicon, purifying it through distillation of trichlorosilane, and using the Siemens process to deposit high purity silicon. Heavy mineral sands can also be separated into minerals like zircon, rut
zeolites, types, nature, synthetic, processes, Deposits and properties;Physical characteristics of some naturally occurring zeolites; molecular sieves;Adsorption and related molecular sieving; zeolite catalysts
This document provides an outline for a lecture presentation on open pit mining methods and planning. It discusses key parameters such as bench height and geometry, cutoff grade calculation, and factors affecting open pit stability. The presentation covers the basic concept of open pit mining, how overburden is removed, and machinery used such as trucks, shovels, and drills. Diagrams illustrate typical bench terminology and pit slope angles. The importance of optimizing the pit design is addressed through considering elements like production scheduling, waste disposal, and ultimate pit limits.
Open pit mining involves digging a large hole or pit at the earth's surface to extract ore deposits near the surface. Overburden or waste rock is removed to expose the ore body, which is then extracted using large excavating equipment like shovels and haul trucks. Ore is transported from the pit either by truck or conveyor belt to a processing facility. Open pit mining provides high productivity and low costs but requires significant capital investment and can have large environmental impacts due to the large scale of surface disturbance. It is best suited to deposits that are relatively shallow and large in area.
Earth Resources
Reserves and resources
Nonrenewable Mineral Resources
What are industrial minerals?
Why are industrial minerals so important?
Geology of Industrial Minerals Deposits
Classification of industrial minerals
General characteristics of Non-metallic Deposits
Factors important in evaluating an industrial minerals deposit
Selected industrial rocks and minerals
ABRASIVES MINERALS
OLIVINE
GYPSUM
CLAY MINERALS
FLUORITE
PERLITE
BUILDING STONES and Rip-rap
CALCIUM CARBONATE DEPOSITS
SULFUR ORE DEPOSITS
CHERT DEPOSITS
PHOSPHATE ORE DEPOSITS
EVAPORITE DEPOSITS
SELECTED SOME NON-METALLIC METAMORPHIC DEPOSITS
Asbestos Deposits
Graphite Deposits
Talc, Soapstone, and Pyrophyllite
Selected Some Ornamental Metamorphic Stones
Marble
Quartzite
Serpentinite
Global discovered resource and yet-to-find, OPEC Countries; Conventional oil and Unconventional oil, UNCONVENTIONAL PROSPECTIVE RESOURCES, Heavy crude oil, Bitumen, Oil sand, Oil shale, Deepwater oil , Polar (ARCTIC) oil , Fractured source rock, Coal liquefaction or Gas to liquids
GROWTH FACTORS AND CHALLENGES FOR OIL MARKET; GROWTH FACTORS FOR OIL MARKET; Demographic Factors, Oil Demand, Motorization in Asian Countries, Upstream Costs Increase, Principal CHALLENGES FOR OIL MARKET, US Shale Oil Production, US shale oil production potential for well drilling, Other constraints, Deepwater Production, Iraqi production growth prospects, GTL – challenge for the oil market after 2020
- The Miocene Epoch lasted from approximately 23 million to 5 million years ago. During this time, grazing animals became more common after the rise of grasses. Both grazers and their predators evolved to be faster to maneuver on the grassy plains.
- A severe drought in the region killed thousands of animals, whose bones were later discovered preserved in river bends after being swept downstream.
- The document discusses the Miocene Epoch in further detail, including the climate and geography at the time as well as notable animals and events.
Phosphorite deposits, Types of Phosphorite deposits , Igneous Phosphate Deposits, Biogenic (or Guano Bird ; or Island) Deposits, Marine Sedimentary Phosphate Deposits, Classification of Phosphatic Sedimentary Marine Rocks, Depositional Environments, Types of Sedimentary Phosphorite Deposition, Nature and Occurrence, Mineralogy and Mineral composition of phosphorite deposit, Origin of Phosphorite, World Phosphate Rock Reserves and Resources, Global Phosphate Rock Production, Use of Phosphate
The document provides information about the Cambrian Period, which began around 543 million years ago and ended around 490 million years ago. It describes the Cambrian Period as a time of the "Cambrian Explosion" when most major animal phyla first appeared in the fossil record over a relatively short period of time. The document outlines the dominant life forms, climate, tectonic setting, stratigraphy, localities, and subdivisions of the Cambrian Period.
Some background on JORC; Why have a JORC Code?, The JORC Code – What is does; JORC a principles based Code; Classification; Stakeholders; 2011 Review of the JORC Code; JORC internationally and its importance.
This document provides an overview of Silver One Resource Inc., a silver exploration and development company. It summarizes Silver One's three key projects: 1) The Candelaria silver project in Nevada, which has a historic resource of over 68 million ounces of silver and is Silver One's flagship project. 2) The Cherokee silver-gold-copper project in Nevada, which has extensive vein systems traced over 12km. 3) The Phoenix Silver project in Arizona, where high-grade silver fragments up to 70% silver have been found. The document discusses Silver One's exploration and development plans over the next 12 months to increase resources and advance projects.
Silver One Resources is a silver exploration company with three highly prospective projects in Nevada and Arizona. The flagship Candelaria Mine Project in Nevada hosts a historic silver resource of over 68 million ounces and has potential for resource expansion through drilling of extensions near the historic pits and exploration of underground high-grade opportunities and porphyry targets. The company is also exploring the extensive epithermal vein system at its Cherokee Project in Nevada over a 12km strike length and has an option to acquire the Phoenix Silver Project in Arizona, where high-grade vein fragments contain up to 70% silver.
This document provides an overview of Silver One Resource Inc., a silver exploration and development company. It summarizes the company's key projects, which include the Candelaria silver project in Nevada, the Cherokee silver-gold-copper project in Nevada, and the Phoenix Silver project in Arizona. It outlines Silver One's strategy to create value through exploration drilling, resource expansion, and advancing projects to production. The document highlights several catalysts for the company over the next 12 months, including planned drilling programs at its key projects to potentially expand mineral resources.
Silver One is a silver exploration and development company with three highly prospective projects in Nevada and Arizona. The company's flagship project is the past-producing Candelaria Mine in Nevada, which hosts a large unexploited historic silver resource that Silver One is targeting through drilling, metallurgical testing, and resource expansion. Silver One also owns the Cherokee silver-gold-copper project in Nevada and has an option to acquire the high-grade Phoenix Silver Project in Arizona, where very high-grade silver fragments have been found. Over the next 12 months, Silver One plans to continue drilling and metallurgical testing at Candelaria, advance exploration at Cherokee, and target the source of the high-grade fragments
This document provides an overview of Silver One Resource Inc., including its flagship Candelaria silver project in Nevada and additional exploration projects. It summarizes:
1) Silver One's goal of building a silver-focused mining company through the exploration and development of its highly prospective silver projects located in Nevada and Arizona.
2) Key details about the Candelaria project, including its past production history, large unexploited historic silver resource, and upcoming exploration plans targeting high-grade opportunities and extensions to known mineralization.
3) Preliminary results from Silver One's 2020-2021 exploration program at Candelaria, which included drilling and geophysical surveys aimed at expanding resources and discovering new mineralized zones.
This document provides an overview of Silver One Resource Inc., a silver exploration and development company. It summarizes the company's key projects, which include the Candelaria silver project in Nevada, the Cherokee silver-gold-copper project in Nevada, and the Phoenix Silver project in Arizona. It outlines Silver One's exploration and development plans over the next 12 months, which include drilling programs to expand resources and test targets at its key projects. The document also reviews silver market fundamentals and why silver is well positioned for future demand growth driven by industrial applications including solar power and electric vehicles.
Silver One Resources Corporate PresentationAdnetNew
This document provides an overview of Silver One Resource Inc., including its flagship Candelaria silver project in Nevada and additional exploration projects. Key points include:
- Silver One is building a silver-focused mining company through the exploration and development of highly prospective silver projects.
- The historic Candelaria Mine in Nevada had past production of 68 million ounces of silver and represents the company's flagship project, with opportunities to create value through heap leach pads, high-grade opportunities, and along-strike potential.
- Additional projects include the Cherokee silver-gold-copper project in Nevada and the high-grade Phoenix Silver Project in Arizona, where vein fragments have returned assays up to 459,000
Within the framework of a new, "substance" (“matter”) paradigm of geophysical research, a "direct" search for a specific physical substance is carried out: gas, oil, gas hydrates, water, ore minerals and rocks (gold, platinum, silver, zinc, uranium, diamonds, kimberlites, etc.). The initial stage in the development of this paradigm can be considered the first research and development on the "direct" methods for oil and gas searching.
This document provides an overview of Silver One Resource Inc., including its flagship Candelaria Mine Project in Nevada. Key points include:
- Silver One has acquired three highly prospective silver-focused projects, including the past-producing Candelaria Mine with a large unexploited historic silver resource.
- The Candelaria Mine had historic production of 68 million ounces of silver and has the potential for heap leach recovery, high-grade opportunities, and resource expansion along strike.
- Silver One is also exploring the Cherokee Project in Nevada and Phoenix Silver Project in Arizona for high-grade silver-gold-copper mineralization along extensive vein systems.
- Upcoming exploration plans include drilling programs
The document discusses Silver One Resource Inc., a silver exploration and development company. It summarizes the company's flagship Candelaria Mine Project in Nevada, which contains a historical silver resource estimate of over 68 million ounces. The project has potential for heap leach processing, high-grade opportunities, and resource expansion. Silver One aims to unlock value at Candelaria through exploration and advancing development work.
Silver One Corporate Presentation Silver Summit October 2018Adnet Communications
Silver One Resources is a silver exploration and development company with assets in Nevada and Mexico. The company's flagship project is the past-producing Candelaria Mine in Nevada, which hosts a historic silver resource. Silver One plans to evaluate opportunities to restart production at Candelaria, including through reprocessing the existing heap leach pads and exploring high-grade areas. The company also owns the Cherokee project in Nevada and Peñasco Quemado project in Mexico, which it will explore for new silver discoveries. Silver One is led by an experienced management team and is well positioned to create value through the advancement of its assets.
The document provides an overview of Silver One Resource Inc., a silver exploration and development company. It summarizes the company's key assets which include the past-producing Candelaria silver mine in Nevada, the Cherokee silver-gold project in Nevada, and the Peñasco Quemado silver project in Mexico. It also discusses the fundamentals of silver as an investment, the undervaluation of silver relative to gold, and Silver One's goal of pursuing potential near-term production opportunities and advancing exploration targets to create shareholder value.
This document provides an overview of the Mineral Exploration and Evaluation course. It discusses the following key topics in mineral exploration:
- Introduction to mineral resources and the historical background of mineral exploration.
- Types, phases and sequences of mineral exploration planning and management.
- Sampling and analytical techniques including sample preparation and laboratory methods.
- Exploration methods such as geological mapping, geochemical and geophysical prospecting.
- Presentation and interpretation of exploration data and resource evaluation including feasibility studies.
It also provides details on various stages of mineral exploration including planning, reconnaissance, follow-up exploration, feasibility studies, construction and mine development, extraction, and mine closure.
Silver One Corporate Presentation - March 2023AdnetNew
The document provides information on Silver One Resources, including its flagship Candelaria Mine Project in Nevada. It summarizes the historic mineral resource estimate reported for the Candelaria Project in 2001, which estimated measured, indicated, and inferred resources. The qualified person has not done sufficient work to classify the historical estimate as a current mineral resource. The document also gives an overview of the company's goals to update resource estimates, conduct economic studies, and continue exploration work with the aim of advancing the Candelaria Project.
Various techniques are used to prospect for mineral deposits, including direct observation, as well as geological, geophysical, and geochemical tools. Once a discovery is made, the prospect is explored to determine characteristics like size, shape, mineral quality distribution, and quantities. Prospecting aims to find anomalies or differences from what would normally be expected through methods like aerial imagery, gravity and magnetic surveys, and analyzing soil, water, and plant samples to identify unusual concentrations. The goal is to delimit areas where valuable mineral resources can be expected to occur based on geological features and prospecting criteria.
This presentation provides an overview of Silver One Resources and its Candelaria Mine Project in Nevada. Some key points:
- Silver One is building a silver-focused mining company through the exploration and development of its projects in Nevada and Arizona.
- The flagship project is the past-producing Candelaria Mine in Nevada, which has a historic silver resource of over 68 million ounces. Silver One is exploring opportunities to expand resources through drilling, metallurgical studies on mineralization and heap leach pads, and economic studies.
- The company's goals over the next 12 months include metallurgical studies and an updated resource estimate at Candelaria, as well as drilling high-grade silver targets at its Phoenix
Geomechanical Modeling Abu Dhabi Commentsssuser886c55
Fractured reservoirs can be categorized into four types based on how fractures impact porosity and permeability. Type 1 reservoirs have fractures providing essential porosity and permeability since the rock matrix has little. Type 2 reservoirs have fractures providing essential permeability with the matrix providing porosity. Type 3 reservoirs have fractures providing additional permeability to an already productive matrix. Type 4 reservoirs have fractures creating barriers rather than improving flow. Recognition of the reservoir type is important for evaluating reserves, predicting production behavior, and designing development plans.
Century Iron Mines Corporation announced its first mineral resource estimate for the Rainy Lake Iron Deposit (Full Moon Deposit) located in Quebec. The estimate includes 7.26 billion tonnes of indicated resources grading 30.18% total iron and 8.69 billion tonnes of inferred resources grading 29.86% total iron. The large, relatively flat deposit has potential to be economically developed due to thick, stratabound iron mineralization. Century plans further exploration and a preliminary economic assessment to evaluate the project's potential.
Resource Estimation and Exploration target generation of Basantgarh Copper-Zi...vishwanath226387
The South-Delhi fold belt has several basemetal prospects and deposits of which the Basantgarh multi-metal deposit occurring in the younger division of Delhi Super group (Ajabgarh Geological investigation in the deposit has established a mineralized strike length of 1000m approximatelyTotal Mineral Resources reported here is 3.28 MT @ 1.92% Cu, 1.37% Zn & 0.18% Pb.s the main mineralization is reported only in the eastern limb of the synform, IP resistivity survey may detect the hidden potential of Basantgarh extension in the western limb.
In the North-Eastern part of the Block, there is an unexplored soil covered area which can be targeted by mobile-metal-Ion for target generation followed by drilling.
Silver One Resources Inc. - Corporate Presentation - May 2022Adnet Communications
This document provides an overview of Silver One Resources and its projects, with a focus on the Candelaria Mine Project in Nevada. It summarizes the history of mining at Candelaria and discusses the historical resource estimate. It outlines Silver One's plans to update the resource estimate to current standards and complete metallurgical and economic studies. Drilling results since 2017 aim to expand resources along strike and at depth and evaluate porphyry potential. The company sees potential to create value through heap leach pads, high-grade opportunities, and expanding the resource along strike from the historic pits.
The objectives of this course in iron ore Resources and iron industry are:
i) acquainting students (majors and non-majors) with the basic tools necessary for studying iron ore deposits and processes,
ii) different processes for phosphorus removal from iron ore
iii) beneficiation processes of iron ore deposits.
iv) different processes and techniques that used to enrichment low-grade iron ore resources
v) understanding the different ironwork processes and technology,
vi) understanding the different types of iron ore products,
vii) prominent routes for steelmaking
viii) understanding the relationship between the distribution of iron ore and scrap, as well as steelmarkets,
ix) steel industry in Egypt , and
x) gaining some knowledge of the global iron ore as well as environmental problems associated with the extraction and utilization of iron ore resources.
There are plenty of hard-to-beneficiate iron ores and high-grade tailings in India and all over the world; As the volume of high-grade iron ores declines.
Minerals phase transformation by hydrogen reduction (MPTH) can efficiently revitalize hard-to-beneficiate iron ore resources and tailings, turning the waste into profitable products. It may also improve the concentrate quality comparing to that from the previous method. From the economic and environmental aspects, MPTH is the most effective method to recover iron oxides.
The clean minerals phase transformation by hydrogen reduction (MPTH) was proposed.
Industrial utilization of limonite/goethite, limonite-hematite, sulfur-bearing refractory iron ore was achieved, where Sulfur-bearing minerals decomposed or formed sulfate after oxidation roasting.
Sulfur content of iron ore concentrate was significantly reduced to 0.038 %.
Improving utilization efficiency of refractory iron ore resources is a common theme for the sustainable development of the world’s steel and iron industry.
Magnetization Roasting is considered as an effective and typical method for the beneficiation of refractory iron ores.
After magnetization roasting, the weakly magnetic iron minerals, including hematite, limonite and siderite, are selectively reduced or oxidized to ferromagnetic magnetite, which is relatively easier to enrich by Magnetic Separation after liberation pretreatments.
The Primary Magnetization Roasting Methods include: Shaft Furnace Roasting, Rotary Kiln Roasting, Fluidized Bed Roasting, and Microwave assisted roasting. The developments in magnetization roasting of difficult to treat iron ores, including: Shaft Furnace Roasting, Rotary Kiln Roasting, Fluidized Bed Roasting, and Microwave Assisted Roasting in the Past Decade.
Shaft Furnace Roasting is gradually eliminated due to its high energy consumption and low industrial processing capacity, and the primary problem for rotary kiln roasting is the kiln coating which affects the yield of iron resource and its industrial application.
Fluidized Bed Roasting and Microwave assisted roasting are considered as the most effective and promising methods.
Suspension (Fluidized) Magnetization Roasting is recognized as the most effective and promising technology due to its high reaction efficiency, low energy consumption and large processing capacity. Moreover, an industrial production line with a throughput of 1.65 million t/a for beneficiation of a specularite ore has been built.
Microwave Assisted Roasting is a potential alternative technology for magnetizing iron ores. However, it is currently limited to laboratory research and has no industrial application. Forwarding microwave assisted magnetization roasting methods into industrial applications needs long way and time to achieve.
Furthermore, using biomass, H2 or siderite as a reducing agent in the magnetic reduction roasting of iron ores is a beneficial way to reduce carbon emissions, which can be called clean and green magnetization roasting technology.
In the future, technical research on clean and green magnetization roasting should be strengthened. Maybe microwave magnetization roasting using biomass/H2/siderite as reductant can be further studied for a more effective and greener magnetization of iron ores.
WORLD RESOURCES IRON DEPOSITS
Iron Ore Pellets Market Industry Trends
Scope and Market Size
Market Analysis and Insights
DRI Production in Plants Using Merchant Iron Ore
Outlook for DR grade pellet supply‐demand out to 2030
DRI and the pathway to carbon‐neutral steelmaking
Supply‐side challenges for the steel & iron ore industries
scrap is the main raw material, is growing in the structure of global steelmaking capacities; SCARP/ RECYCLING IRON ; EAF steel production method in the world; Scrap for Stock; A Global Scrap Shortage;Availability of Ferrous Scrap Resources; EGYPT IRON SCRAP IMPORTS.
The iron ore production has significantly expanded in recent years, owing to increasing steel demands in developing countries.
However, the content of iron in ore deposits has deteriorated and low-grade iron ore has been processed.
The fine ores resulting from the concentration process must be agglomerated for use in iron and steelmaking.
Bentonite is the most used binder due to favorable mechanical and metallurgical pellet properties, but it contains impurities especially silica and alumina.
Better quality wet, dry, preheated, and fired pellets can be produced with combined binders, such as organic and inorganic salts, when compared with bentonite-bonded pellets.
While organic binders provide sufficient wet and dry pellet strengths, inorganic salts provide the required preheated and fired pellet strengths.
The industrial development program of any country, by and large, is based on its natural resources.
Currently the majority of the world’s steel is produced through either one of the two main routes: i) the integrated Blast Furnace – Basic Oxygen Furnace (BF – BOF) route or ii) the Direct Reduced Iron - Electric Arc Furnace (DRI - EAF) route.
Depleting resources of coking coal, the world over, is posing a threat to the conventional (Blast Furnace [Bf]–Basic Oxygen Furnace [BOF]) route of iron and steelmaking.
During the last four decades, a new route of ironmaking has rapidly developed for Direct Reduction (DR) of iron ore to metallic iron by using noncoking coal/natural gas.
This product is known as Direct Reduced Iron (DRI) or Sponge Iron.
Processes that produce iron by reduction of iron ore (in solid state) below the melting point are generally classified as DR processes.
Based on the types of reductant used, DR processes can be broadly classified into two groups: (1) coal-based DR process and (2) gas-based DR process.
Details of DR processes, reoxidation, storage, transportation, and application of DRI are discussed in this presentation.
This presentation reviews the different DR processes used to produce Direct Reduced Iron (DRI), providing an analysis on the quality requirements of iron-bearing ores for use in these processes. The presentation also discusses the environmental sustainability of such processes. DR processes reduce iron ore in its solid state by the use of either natural gas or coal as reducing agents, and they have a comparative advantage of low capital costs, low emissions and production flexibility over the BF process.
Currently the majority of the world’s steel is produced through either one of the two main routes: i) the integrated Blast Furnace – Basic Oxygen Furnace (BF – BOF) route or ii) the Direct Reduced Iron - Electric Arc Furnace (DRI - EAF) route.
In the former, the blast furnace uses iron ore, scrap metal, coke and pulverized coal as raw materials to produce hot metal for conversion in the BOF. Although it is still the prevalent process, blast furnace hot metal production has declined over the years due to diminishing quality of metallurgical coke, low supply of scrap metal and environmental problems associated with the process. These factors have contributed to the development of alternative technologies of ironmaking, of which Direct Reduction (DR) processes are expected to emerge as preferred alternatives in the future.
This presentation reviews the different DR processes used to produce Direct Reduced Iron (DRI), providing an analysis on the quality requirements of iron-bearing ores for use in these processes. The presentation also discusses the environmental sustainability of such processes. DR processes reduce iron ore in its solid state by the use of either natural gas or coal as reducing agents, and they have a comparative advantage of low capital costs, low emissions and production flexibility over the BF process.
Ironmaking represents the first step in steelmaking.
The iron and steel industry is the most energy-intensive and capital-intensive manufacturing sector in the world (Strezov, 2006).
Steelmaking processes depend on different forms of iron as primary feed material. Traditionally, the main sources of iron for making steel were Blast Furnace hot metal and recycled steel in the form of scrap.
The Blast Furnace (BF) has remained the workhorse of worldwide virgin iron production (i.e., hot metal) for more than 200 years. Over the years, BFs have evolved into highly efficient chemical reactors, capable of providing stable operation with a wide range of feed materials.
However, operation of modern efficient BFs normally involves sintering and coke making and their associated environmental problems.
More than 90% of iron is currently produced via the BF process, while the rest is coming from Direct Reduction (DR) processes, Mini Blast Furnaces (MBFs), Corex, Finex, Ausmelt, etc. Additionally, the severe shortage of good-quality metallurgical coal has remained an additional constraint all over the world. In view of this, there is an increasing awareness that the BF route needs to be supplemented with alternative ironmaking processes that are more environment friendly and less dependent on metallurgical coal.
The document discusses reduction roasting followed by magnetic separation as a promising technique for enriching iron values from low-grade iron ores. It provides an overview of the technique, noting that reduction roasting involves reducing hematite and goethite phases in iron ores to magnetite, which can then be separated magnetically. The document reviews reduction roasting studies on various types of low-grade iron ores, including oolitic iron ores, banded iron ores, iron ore slimes and tailings. Emerging trends in reduction roasting such as microwave-assisted and biomass-assisted methods are also examined.
Phosphorus removal from iron ore is important for efficient steelmaking. Various processes have been developed to reduce phosphorus levels prior to smelting, including physical separation techniques that leverage differences in particle properties, and chemical/hydrometallurgical methods utilizing reagents to selectively remove or transform phosphorus. Further optimization is needed to improve phosphorus removal efficiency and minimize environmental impacts.
Overview of IRON TYPES: Pig Iron, Direct Reduced Iron (DRI), Hot Briquetted Iron (HBI), Cold Briquetted Iron (CBI) and Cold Briquetted Iron and Carbon (CBIC) Specifications .
Comparison of Pig Iron and DRI
Properties; Manufacturing Process; Uses; Largest producers and markets
Iron ore mining plays a critical role in supplying the raw material necessary for steel production, supporting various industries and economic development worldwide.
From the extraction of iron ore to its processing and eventual export, each stage of the mining process requires careful planning, technological advancements, and environmental considerations.
By adopting sustainable mining practices and mitigating environmental impacts, the future of iron ore mining can be aligned with the principles of responsible resource utilization and environmental stewardship
The Egyptian steel sector is the second largest steel market in the Middle East and North Africa region in terms of production and third largest in terms of consumption.
Egypt was the third-ranked producer of Direct-Reduced Iron (DRI) in the Middle east and North Africa region after Iran and Saudi Arabia and accounted for 5.4% of the world’s total output
The Egyptian steel industry represents one of the cornerstones of Egypt’s economic growth and development, due to its linkages to almost all other industries that stimulate economic expansion, such as construction, housing, infrastructure, consumer goods and automotive. All these industries rely heavily on steel industry and so, the importance and development of the steel sector is significant for the progress of the Egyptian economy in general.
The Egyptian market has many companies that produce different steel products.
This document provides the curriculum vitae of Prof. Dr. Hassan Zakaria Harraz. It details his personal and academic background, including his education, positions held, research interests, and publications. He is currently a professor of economic geology and ore resources at Tanta University in Egypt. The CV outlines his extensive experience in economic geology, mineral exploration, and research focused on gold deposits in Egypt. It also lists over 30 of his published papers on related topics.
Exploration in Deep Weathering Profiles, Supergene, R-mode factor analysis; Multi-element association geochemistry; Assessment of Au-Zn potentiality in Gossan; Rodruin-Egypt
Mineral Processing: Crusher and Crushing; Secondary and Tertiary Crushing Circuits; Types of Crusher; Types of Crushing; Types of Jaw Crushers; Impact Crusher; Types of Cone Crushers; Ball Mill; BEST STONE MANUFACTURERS; Local Quality and High quality ; International and Country/Hand made
Classification Equipment
Introduction; Chemical composition of garnet; Structure; Classification; Physical properties; Optical properties; Occurrences; Gem variety; and Uses
Garnet group of minerals is one of the important group of minerals.
Since they are found in wide variety of colours, they are also used as gemstones.
Garnet group of minerals are also abrasives and thus have various industrial applications.
The cost of acquiring information by natural selectionCarl Bergstrom
This is a short talk that I gave at the Banff International Research Station workshop on Modeling and Theory in Population Biology. The idea is to try to understand how the burden of natural selection relates to the amount of information that selection puts into the genome.
It's based on the first part of this research paper:
The cost of information acquisition by natural selection
Ryan Seamus McGee, Olivia Kosterlitz, Artem Kaznatcheev, Benjamin Kerr, Carl T. Bergstrom
bioRxiv 2022.07.02.498577; doi: https://doi.org/10.1101/2022.07.02.498577
Immersive Learning That Works: Research Grounding and Paths ForwardLeonel Morgado
We will metaverse into the essence of immersive learning, into its three dimensions and conceptual models. This approach encompasses elements from teaching methodologies to social involvement, through organizational concerns and technologies. Challenging the perception of learning as knowledge transfer, we introduce a 'Uses, Practices & Strategies' model operationalized by the 'Immersive Learning Brain' and ‘Immersion Cube’ frameworks. This approach offers a comprehensive guide through the intricacies of immersive educational experiences and spotlighting research frontiers, along the immersion dimensions of system, narrative, and agency. Our discourse extends to stakeholders beyond the academic sphere, addressing the interests of technologists, instructional designers, and policymakers. We span various contexts, from formal education to organizational transformation to the new horizon of an AI-pervasive society. This keynote aims to unite the iLRN community in a collaborative journey towards a future where immersive learning research and practice coalesce, paving the way for innovative educational research and practice landscapes.
(June 12, 2024) Webinar: Development of PET theranostics targeting the molecu...Scintica Instrumentation
Targeting Hsp90 and its pathogen Orthologs with Tethered Inhibitors as a Diagnostic and Therapeutic Strategy for cancer and infectious diseases with Dr. Timothy Haystead.
Describing and Interpreting an Immersive Learning Case with the Immersion Cub...Leonel Morgado
Current descriptions of immersive learning cases are often difficult or impossible to compare. This is due to a myriad of different options on what details to include, which aspects are relevant, and on the descriptive approaches employed. Also, these aspects often combine very specific details with more general guidelines or indicate intents and rationales without clarifying their implementation. In this paper we provide a method to describe immersive learning cases that is structured to enable comparisons, yet flexible enough to allow researchers and practitioners to decide which aspects to include. This method leverages a taxonomy that classifies educational aspects at three levels (uses, practices, and strategies) and then utilizes two frameworks, the Immersive Learning Brain and the Immersion Cube, to enable a structured description and interpretation of immersive learning cases. The method is then demonstrated on a published immersive learning case on training for wind turbine maintenance using virtual reality. Applying the method results in a structured artifact, the Immersive Learning Case Sheet, that tags the case with its proximal uses, practices, and strategies, and refines the free text case description to ensure that matching details are included. This contribution is thus a case description method in support of future comparative research of immersive learning cases. We then discuss how the resulting description and interpretation can be leveraged to change immersion learning cases, by enriching them (considering low-effort changes or additions) or innovating (exploring more challenging avenues of transformation). The method holds significant promise to support better-grounded research in immersive learning.
The binding of cosmological structures by massless topological defectsSérgio Sacani
Assuming spherical symmetry and weak field, it is shown that if one solves the Poisson equation or the Einstein field
equations sourced by a topological defect, i.e. a singularity of a very specific form, the result is a localized gravitational
field capable of driving flat rotation (i.e. Keplerian circular orbits at a constant speed for all radii) of test masses on a thin
spherical shell without any underlying mass. Moreover, a large-scale structure which exploits this solution by assembling
concentrically a number of such topological defects can establish a flat stellar or galactic rotation curve, and can also deflect
light in the same manner as an equipotential (isothermal) sphere. Thus, the need for dark matter or modified gravity theory is
mitigated, at least in part.
hematic appreciation test is a psychological assessment tool used to measure an individual's appreciation and understanding of specific themes or topics. This test helps to evaluate an individual's ability to connect different ideas and concepts within a given theme, as well as their overall comprehension and interpretation skills. The results of the test can provide valuable insights into an individual's cognitive abilities, creativity, and critical thinking skills
Current Ms word generated power point presentation covers major details about the micronuclei test. It's significance and assays to conduct it. It is used to detect the micronuclei formation inside the cells of nearly every multicellular organism. It's formation takes place during chromosomal sepration at metaphase.
Authoring a personal GPT for your research and practice: How we created the Q...Leonel Morgado
Thematic analysis in qualitative research is a time-consuming and systematic task, typically done using teams. Team members must ground their activities on common understandings of the major concepts underlying the thematic analysis, and define criteria for its development. However, conceptual misunderstandings, equivocations, and lack of adherence to criteria are challenges to the quality and speed of this process. Given the distributed and uncertain nature of this process, we wondered if the tasks in thematic analysis could be supported by readily available artificial intelligence chatbots. Our early efforts point to potential benefits: not just saving time in the coding process but better adherence to criteria and grounding, by increasing triangulation between humans and artificial intelligence. This tutorial will provide a description and demonstration of the process we followed, as two academic researchers, to develop a custom ChatGPT to assist with qualitative coding in the thematic data analysis process of immersive learning accounts in a survey of the academic literature: QUAL-E Immersive Learning Thematic Analysis Helper. In the hands-on time, participants will try out QUAL-E and develop their ideas for their own qualitative coding ChatGPT. Participants that have the paid ChatGPT Plus subscription can create a draft of their assistants. The organizers will provide course materials and slide deck that participants will be able to utilize to continue development of their custom GPT. The paid subscription to ChatGPT Plus is not required to participate in this workshop, just for trying out personal GPTs during it.
EWOCS-I: The catalog of X-ray sources in Westerlund 1 from the Extended Weste...Sérgio Sacani
Context. With a mass exceeding several 104 M⊙ and a rich and dense population of massive stars, supermassive young star clusters
represent the most massive star-forming environment that is dominated by the feedback from massive stars and gravitational interactions
among stars.
Aims. In this paper we present the Extended Westerlund 1 and 2 Open Clusters Survey (EWOCS) project, which aims to investigate
the influence of the starburst environment on the formation of stars and planets, and on the evolution of both low and high mass stars.
The primary targets of this project are Westerlund 1 and 2, the closest supermassive star clusters to the Sun.
Methods. The project is based primarily on recent observations conducted with the Chandra and JWST observatories. Specifically,
the Chandra survey of Westerlund 1 consists of 36 new ACIS-I observations, nearly co-pointed, for a total exposure time of 1 Msec.
Additionally, we included 8 archival Chandra/ACIS-S observations. This paper presents the resulting catalog of X-ray sources within
and around Westerlund 1. Sources were detected by combining various existing methods, and photon extraction and source validation
were carried out using the ACIS-Extract software.
Results. The EWOCS X-ray catalog comprises 5963 validated sources out of the 9420 initially provided to ACIS-Extract, reaching a
photon flux threshold of approximately 2 × 10−8 photons cm−2
s
−1
. The X-ray sources exhibit a highly concentrated spatial distribution,
with 1075 sources located within the central 1 arcmin. We have successfully detected X-ray emissions from 126 out of the 166 known
massive stars of the cluster, and we have collected over 71 000 photons from the magnetar CXO J164710.20-455217.
2. 2
The Russian Code
Currently effective in Russia is the Code approved by the
Decree of the Ministry of Natural Resources, RF № 278 of
11 December, 2006.
Full title of the Document:
Classification of resources/reserves and prognostic resources of
solid minerals
3. 3
The Russian Code (continued)
The purpose of the Code – defining the principles of calculation,
assessment and keeping state Inventory of mineral wealth being also
the foundation of planning and forecasting.
Calculation and taking account of reserves/resources, estimation and
taking account of undiscovered resources is done in mass measures
in compliance with economically justified cut-off parameters, with no
account taken of ore losses and dilution in mining, concentration
and processing minerals.
4. 4
The Russian Code (continued)
Contents of the Russian Code:
I. Generalities.
II. Groups of mineral reserves by economic viability.
III. Reserve and prognostic resource categories by
geological exploration knowledge.
IV. Groups of mineral deposits by geological complexity.
V. Groups of mineral reserves by maturity for production.
5. 5
The Russian Code (continued)
Reserves/Resources Undiscovered (prognostic) resources
Groups by maturity for production
Developed (feasibility study based
on permanent cut-off grades)
А,В,С1,С2
Estimated (feasibility based on
of tentative cut-off grades)
С2 (С1)
Increase of geological knowledge, economic and technological substantiation
Reserve categories by geological exploration knowledge
А В С1 С2 Р1 Р2 Р3
Resource categories by degree of geological
substantiation
Groups by economic viability
On-balance (economic)
Out-of-balance (potentially
economic)
6. 6
Assessment of undiscovered resources and reserves of
mineral deposits by stages of exploration
Stage
Targets of
studies/assessment
Kind of geological-
economic assessment
Categories
Degree of maturity
for production
1.
Regional geological
studies
Metallogenic zones,
basins, ore regions &
fields
- Р3, Р2
-
2. Prospecting
Ore fields &
occurrences
Technical-economic
justification
Р1
-
3.
Estimation of
mineral deposits
Mineral deposits
Feasibility study of
tentative cut-off grades
С2 (С1) Estimated
4.
Development of
mineral deposits
Mineral deposits, ore
accumulations, ore
bodies
Feasibility study of
permanent cut-off
grades
А, В, С1,С2
Developed
Increaseofgeologicalknowledge,
economic&technologicalsubstantiation
7. 7
Groups by maturity for production
Developed (feasibility study based
on permanent cut-off grades)
А,В,С1,С2
Estimated (feasibility based on
of tentative cut-off grades)
С2 (С1)
The Russian Code. Groups of reserves by economic
viability.
Reserves/Resources Undiscovered (prognostic) resources
Increase of geological knowledge, economic and technological substantiation
Reserve categories by geological exploration knowledge
А В С1 С2 Р1 Р2 Р3
Resource categories by degree of geological
substantiation
Groups by economic viability
On-balance (economic)
Out-of-balance (potentially
economic)
8. 8
Subdividing reserves by economic viability
Reserves Conditions of defining
On-balance (economic)
Economic efficiency of recovery by up-to-date technical &
technological level of mining development is proved by technical
and economic feasibility calculations with rational use of subsoil
and environmental requirements taken into account.
Out-of-balance
(potentially economic)
Mining in present day conditions is not feasible for various
reasons.
Economic, technological, geotechnical and other prerequisits are
available for the reserve to be used in the near prospective.
The possibility of extraction and storing for further use is proved.
9. 9
The Russian Code. Groups of reserves by degree of
maturity for production
Reserves/Resources Undiscovered (prognostic) resources
Increase of geological knowledge, economic and technological substantiation
Reserve categories by geological exploration knowledge
А В С1 С2 Р1 Р2 Р3
Resource categories by degree of geological
substantiation
Groups by economic viability
On-balance (economic)
Out-of-balance (potentially
economic)
Groups by maturity for production
Developed (feasibility study based
on permanent cut-off grades)
А,В,С1,С2
Estimated (feasibility based on
of tentative cut-off grades)
С2 (С1)
10. 10
Subdividing reserves by degree of maturity for
production
Groups of reserves Conditions of defining
Developed
Reserves: quality,
metallurgy, hydrological
and geotechnical
conditions of exploitation
are studied:
- by drill holes and underground
workings with completeness
sufficient for elaborating technical-
economic study of bringing them
into production.
Estimated
- to the extent sufficient to justify
further development studies and trial
commercial recovery.
11. 11
Groups by maturity for production
Developed (feasibility study based
on permanent cut-off grades)
А,В,С1,С2
Estimated (feasibility based on
of tentative cut-off grades)
С2 (С1)
The Russian Code. Categories of reserves by degree of
geological knowledge.
Reserves/Resources Undiscovered (prognostic) resources
Increase of geological knowledge, economic and technological substantiation
Р1 Р2 Р3
Resource categories by degree of geological
substantiation
Groups by economic viability
On-balance (economic)
Out-of-balance (potentially
economic)
Reserve categories by geological exploration knowledge
А В С1 С2
12. 12
Subdividing reserves by degree of geological
knowledge
Defining reserves in А, В, С1 и С2 categories is carried out by
degree of detail and assurance of studying:
shape,
size,
bedding conditions,
regular features of internal structure,
natural varieties,
technological types and other characteristics of mineral bodies.
“A” category is distinguished by the highest level of confidence, C2
by the lowest one.
13. 13
Grouping mineral deposits by complexity
№
Properties
Description of properties of subdividing reserves by geological complexity
groups
Group I Group II Group III Group IV
1. Size and shape
features
Large, medium
size, bedded,
stratiform,
lenticular
Large, medium size,
bedded, stratiform,
lenticular,
stockworks, pipes
Medium- and
small-size,
stratiform,
lenticular,
stockworks, lodes,
pipes
Small, more seldom
medium-size, lenses,
pipes
2. Variability of
thickness and
Steady Variable Very variable Sharply variable
internal
structure
Simple Complicated Very complicated Extraordinarily
complicated
3. Bedding
disturbances by
tectonics
Not disturbed,
weakly disturbed Disturbed
Intensively
disturbed
Intensively disturbed
4. Uniformity of
distribution of
valuable
components
Even Uneven Very uneven Discontinuous, nest-like
14. 14
Quantitative characteristics of variability of main
properties of mineral bodies
Groups of deposits
Measures of variability of development targets
Shape Grade
Кr q Vm, % Vc, %
1st 0,9–1,0 0,8–0,9 40 40
2nd 0,7–0,9 0,6–0,8 40–100 40–100
3rd 0,4–0,7 0,4–0,6 100–150 100–150
4th 0,4 0,4 150 150
Кr - Ore content ratio
q - Index of complexity
Vm - Thickness variation ratio
Vc - Grade variation ratio (in ore intersections)
15. 15
Grouping mineral deposits by complexity groups is often used at early exploration stages for choosing parameters of
exploration grids and qualifying mineral reserves by exploration results.
Generalized information on exploration workings grid
densities applied in development of tungsten (W) deposits
Group
Characteristics of ore bodies
Type of
workings
Spacing between ore intersections in exploration workings for reserve categories, m
А В С1
On strike On dip On strike On dip On strike On dip
1st
Large stockworks of simple shape and
structure with relatively uniform
distribution of WO3
Adits, drifts – 60–80 – – – –
Orts, crosscuts 50–60 – – – – –
Rises 100–120 – – – – –
Drill holes – – 100–120 100–120 120–200 120–200
2nd
Large stockworks, skarn bodies of
complicated morphology or with
uneven distribution of WO3
Adits, drifts – – – 60–80 – –
Orts, crosscuts – – 50–60 – – –
Rises – – 100-120 – – –
Drill holes – – 50–60 50–60 100–120 100–120
Large lodes or mineralized zones
predominantly steeply dipping with
unsteady thickness and uneven
distribution of WO3
Adits, drifts – – – 60–80 – –
Orts, crosscuts – – 20–30 – – –
Rises – – 100–120 – – –
Drill holes – – 60–80 40–50 100–120 60–80
3rd
Medium size lodes, complex
stratiform, lens-shaped and lenticular
skarn accumulations with unsteady
thickness and very uneven distribution
of WO3
Adits, drifts – – – – – 40–60
Orts, crosscuts – – – – 10–20 –
Rises – – – – 60–120 –
Drill holes – – – – 60–80 40–50
16. 16
Generalized information on exploration workings grid
densities applied in development of deposits of
radioactive metals
Groups Mineral body types
Types of
workings
Spacing between ore intersections in exploration workings
for reserve categories, m.
В С1
On strike On dip On strike On dip
2nd
Bedded, lens-shaped on a plan, with steady thickness
and continuously low grades.
Drill holes 200–100 50–25 200–100 100–50
Large, steeply dipping, high continuity lodes with
uneven grade distribution.
Drifts – 120–60 – –
Orts 25–10 25–10 – –
Rises 120 – – –
Drill holes – – 200–100 100–50
3rd
Veinlike and stockworks, steeply dipping, of medium
continuity and very uneven grade distribution.
Drifts – – – 60–80
Orts – – 50–25 25–10
Rises – – 40–60 –
Drill holes 50–25 25–10
Stratiform, of medium and high continuity and uneven
grade distribution.
Drifts – – – 60–120
Orts – – 50–25 50–25
Drill holes – – 100–50 50–25
Stratiform, ribbon-like, of high continuity on a plan and
low in vertical section, with relatively uniform grade
distribution.
Drill holes – – 200–100 50–25
4th Vein- and pipe-like bodies of low continuity with
extraordinarily uneven grade distribution.
Drifts – – – 40–60
Orts – – 25–10 25–10
Rises – – 40–60 –
17. 17
Groups by maturity for production
Developed (feasibility study based
on permanent cut-off grades)
А,В,С1,С2
Estimated (feasibility based on
of tentative cut-off grades)
С2 (С1)
The Russian Code. Resource categories by degree of
geological substantiation.
Reserves/Resources Undiscovered (prognostic) resources
Increase of geological knowledge, economic and technological substantiation
Reserve categories by geological exploration knowledge
А В С1 С2
Groups by economic viability
On-balance (economic)
Out-of-balance (potentially
economic)
Р1 Р2 Р3
Resource categories by degree of geological
substantiation
18. 18
Classification of resources by degree of geological
knowledge
Main factors of distinguishing resource categories
Р1 Р2 Р3
Possibility of expanding
boundaries of mineralization
beyond the limits of C2 reserves or
identifying new ore bodies in
occurrences, deposits explored and
under exploration by geological,
geophysical and geochemical data,
on materials obtained in structural
and appraisal drill holes.
Possibility of discovery of new
deposits in a basin, ore region,
knot, ore field by data of large
scale surveying and prospecting
on mineral occurrences,
geophysical and geochemical
anomalies.
Potential of discoveries of mineral
deposits based on favorable
geological and paleogeological
prerequisites by data of geological/
geophysical and mapping surveying,
interpretation of space images,
analysis of results obtained by
geophysical and geochemical
investigations.
When defining resource categories the following factors are taken into
consideration: