India has significant iron ore deposits distributed across several states. The major types of iron ore formations in India are banded iron formations from the Precambrian era and laterite ores derived from sub-aerial weathering. The key iron ore minerals are magnetite, hematite, siderite and limonite. India's major iron ore mining districts are located in Odisha, Jharkhand, Chhattisgarh, Karnataka, Goa and other states. These deposits were formed by various geological processes including chemical precipitation in ancient sedimentary basins, weathering of parent rocks, magmatic activity and hydrothermal mineralization.
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.
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.
Metallogenic Epoch and Province
Metallogenetic Epochs
Metallogenetic epochs, as defined above, are specific periods characterised by formation of large number of mineral deposits. It does not mean that all the mineral deposits formed during a definite metallogenetic epochs. In India the chief metallogenetic epochs were:
1. Precambrian
2. Late Palaeozoic
3. Late Mesozoic to Early Tertiary
GEOLOGICAL THERMOMETERS
DEFINITION AND CLASSIFICATION
Proper understanding of origin of mineral deposits and their classification requires the knowledge of formation-temperatures of these deposits. Certain minerals, present over there, give information’s with regard to temperatures of their formations and of the enclosing deposits and they are known as geological thermometers. These geological thermometers may be classed chiefly into the following groups based on their preciseness:
1. The thermometers that record fairly accurately the specific temperature condition of formation of deposits.
2. The thermometers that provide an upper or a lower temperature, above or below which the deposits do not form
3. The thermometers that provide a range of temperature within which the deposits form; and
4. The thermometers that serve as rough indications of temperatures of formation of mineral deposits.
The presence of two or more of less precise geological thermometers in a deposit narrows the range of temperature of formation for the deposits
How can minerals deposits be formed; GEOLOGICAL PROCESSES; Ore Fluids; Ore Forming Processes; Concentrating Processes; Magmatic mineral deposits; Residual mineral deposits ; Placer deposits; Sedimentary mineral deposits; Metamorhogenic mineral deposits; Hydrothermal mineral deposits ; Magmatic Deposits
Cumulate deposits: fractional crystallization processes can concentrate metals (Cr, Fe, PGE, Pt, Ni, Ti, Diamond ))
Pegmatites : late staged crystallization forms pegmatites and many residual elements are concentrated (Li, Ce, Be, Sn, U, Rare Earths (REE), Feldspar, Mica, Gems).
magmatic deposits; Mode of Formation of Magmatic Ores Deposits; Mode of Formation of Orthomagmatic Ores ; Fractional Crystallization (or Crystal fractionation ); Magmatic (or Liquid ) Immiscibility; Simple crystallization without concentration (Dissemination); Segregation of early formed crystals; (Layer Types); Injection of material concentrated elsewhere by differentiation Residual liquid segregation; Residual liquid injection; Immiscible liquid segregation; Immiscible-liquid-injection; Early magmatic deposit; Late magmatic deposit; Types of Magmatic Ore Deposits:Chromite; Fe-Ti (± V) oxides; Ni – Cu – Fe (± Pt) sulfides; Platinum Group Elements (PGEs); REE, and Zr in Carbonatites; Diamond in kimberlites.
Metallogenic Epoch and Province
Metallogenetic Epochs
Metallogenetic epochs, as defined above, are specific periods characterised by formation of large number of mineral deposits. It does not mean that all the mineral deposits formed during a definite metallogenetic epochs. In India the chief metallogenetic epochs were:
1. Precambrian
2. Late Palaeozoic
3. Late Mesozoic to Early Tertiary
GEOLOGICAL THERMOMETERS
DEFINITION AND CLASSIFICATION
Proper understanding of origin of mineral deposits and their classification requires the knowledge of formation-temperatures of these deposits. Certain minerals, present over there, give information’s with regard to temperatures of their formations and of the enclosing deposits and they are known as geological thermometers. These geological thermometers may be classed chiefly into the following groups based on their preciseness:
1. The thermometers that record fairly accurately the specific temperature condition of formation of deposits.
2. The thermometers that provide an upper or a lower temperature, above or below which the deposits do not form
3. The thermometers that provide a range of temperature within which the deposits form; and
4. The thermometers that serve as rough indications of temperatures of formation of mineral deposits.
The presence of two or more of less precise geological thermometers in a deposit narrows the range of temperature of formation for the deposits
How can minerals deposits be formed; GEOLOGICAL PROCESSES; Ore Fluids; Ore Forming Processes; Concentrating Processes; Magmatic mineral deposits; Residual mineral deposits ; Placer deposits; Sedimentary mineral deposits; Metamorhogenic mineral deposits; Hydrothermal mineral deposits ; Magmatic Deposits
Cumulate deposits: fractional crystallization processes can concentrate metals (Cr, Fe, PGE, Pt, Ni, Ti, Diamond ))
Pegmatites : late staged crystallization forms pegmatites and many residual elements are concentrated (Li, Ce, Be, Sn, U, Rare Earths (REE), Feldspar, Mica, Gems).
magmatic deposits; Mode of Formation of Magmatic Ores Deposits; Mode of Formation of Orthomagmatic Ores ; Fractional Crystallization (or Crystal fractionation ); Magmatic (or Liquid ) Immiscibility; Simple crystallization without concentration (Dissemination); Segregation of early formed crystals; (Layer Types); Injection of material concentrated elsewhere by differentiation Residual liquid segregation; Residual liquid injection; Immiscible liquid segregation; Immiscible-liquid-injection; Early magmatic deposit; Late magmatic deposit; Types of Magmatic Ore Deposits:Chromite; Fe-Ti (± V) oxides; Ni – Cu – Fe (± Pt) sulfides; Platinum Group Elements (PGEs); REE, and Zr in Carbonatites; Diamond in kimberlites.
International Journal of Engineering Research and DevelopmentIJERD Editor
Electrical, Electronics and Computer Engineering,
Information Engineering and Technology,
Mechanical, Industrial and Manufacturing Engineering,
Automation and Mechatronics Engineering,
Material and Chemical Engineering,
Civil and Architecture Engineering,
Biotechnology and Bio Engineering,
Environmental Engineering,
Petroleum and Mining Engineering,
Marine and Agriculture engineering,
Aerospace Engineering.
A Simple PPT that helps teachers share the lesson on Minerals and Energy Resources of NCERT a little better and more easily and effectively. Feedbacks are welcome
Iron is the most vital metal in human use. It constitutes 5.05% of the crust material and holds third position in abundance after silicon and aluminium. It is rarely found in native condition except in meteorites and some eruptive rocks. It enters into large number of rocks forming silicates and is widely available as oxides. The mineral containing iron must be mineable at profit in order to be called an 'iron-ore.' The total world production of iron-ore in 1990 was about 1,008 million tonnes (Economic Geology - Umeshwar Prasad) to which India's contribution was about 55.5 million tonnes (contributing 5.5%) with 6th position in the world production.
Boiling Point: 5182°F (2862°C) Atomic Symbol: Fe
Melting Point: 2800°F (1538°C) Atomic Number: 26
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
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2024.06.01 Introducing a competency framework for languag learning materials ...Sandy Millin
http://sandymillin.wordpress.com/iateflwebinar2024
Published classroom materials form the basis of syllabuses, drive teacher professional development, and have a potentially huge influence on learners, teachers and education systems. All teachers also create their own materials, whether a few sentences on a blackboard, a highly-structured fully-realised online course, or anything in between. Despite this, the knowledge and skills needed to create effective language learning materials are rarely part of teacher training, and are mostly learnt by trial and error.
Knowledge and skills frameworks, generally called competency frameworks, for ELT teachers, trainers and managers have existed for a few years now. However, until I created one for my MA dissertation, there wasn’t one drawing together what we need to know and do to be able to effectively produce language learning materials.
This webinar will introduce you to my framework, highlighting the key competencies I identified from my research. It will also show how anybody involved in language teaching (any language, not just English!), teacher training, managing schools or developing language learning materials can benefit from using the framework.
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He discussed the concept of quality improvement, emphasizing its applicability to various aspects of life, including personal, project, and program improvements. He defined quality as doing the right thing at the right time in the right way to achieve the best possible results and discussed the concept of the "gap" between what we know and what we do, and how this gap represents the areas we need to improve. He explained the scientific approach to quality improvement, which involves systematic performance analysis, testing and learning, and implementing change ideas. He also highlighted the importance of client focus and a team approach to quality improvement.
Read| The latest issue of The Challenger is here! We are thrilled to announce that our school paper has qualified for the NATIONAL SCHOOLS PRESS CONFERENCE (NSPC) 2024. Thank you for your unwavering support and trust. Dive into the stories that made us stand out!
2. o Introduction
o Mineralogy
o Types of iron ore formation and
deposits
o Distribution and occurrence
o Conclusion
o Reference
3. Introduction
o Iron is the most indispensable mineral to
man
o It is the second largest element in the
earth’s crust
o Iron is the most abundant metallic element
in the earth’s crust and accounts for 5-6%
of the lithosphere
o Usually it is combined with other elements
such as oxygen and sulphur
o Iron and steel contribute one of the
foundations for modern industrial
civilization
6. Types of iron formations
Gross in 1965 identified two types of iron formations from
the pre-cambrian, they are:
o Algoma type :
Dominant in Archean age and characterized by thin banding
and absence of oolitic and granular texture
Closely associated with volcanic and greywacke sediments
o Superior type :
Characteristic formation of Proterozoic age
Closely associated with clastic sediments like quartzite,
dolomite and pelitic rocks without showing an direct
relation with volcanic association
7. Origin and classification of Iron ore deposits:
The iron ore deposits of India can be broadly divided in to
the following six groups on the basis of mode of
occurrence and origin:
o Banded Iron Formation of Pre-Cambrian Age
o Sedimentary iron ore deposits of siderite and limonitic
composition
o Laterite ores derived from the sub-aerial alterations
o Ores formed by magmatic activity
o Titaniferous and vanadiferous magnetites
o Fault and fissure filling deposits
8. 1. Banded Iron Formation of Pre-Cambrian Age:
The BIF deposits is very well developed in India. The most
common names used are Banded Haematite Quartzite
(BHQ) and Banded Magnetite Quartzite (BMQ).
This belong to Dharwar group of meta-volcanics and
metasediments.
These banded formations were probably formed as
chemical precipitates in partially enclosed sedimentary
basins of back water type.
9. 2. Sedimentary iron ore deposits of siderite and limonitic
composition:
It is also known as Bog iron deposit.
These ores of siderite and limonitic compositions are
found associated with the iron stone shales of lower
Gondwana age
The iron minerals are accumulated as irregular bodies in
stream beds and typically at the bottom levels of bogs and
marshes where lower Gondwana sediments have deposited
along with their organic debris.
10. 3. Laterite ores derived from the sub-aerial
alterations:
Laterite types of iron ores are derived from the sub-aerial
alteration of rocks, such as gneisses, schists, basic lava
under humid tropical conditions.
The ores are generally concentrated at the top as a
resultant alteration product of the iron bearing parent
rocks and consist of oxidised and insoluble rock
constituents.
11. 4. Ores formed by magmatic activity:
A zone of apatite-magnetite rock is found closely
associated with the copper belt of Singhbhum.
These are supposed to have been formed by magmatic
activity associated with pre-Cambrian diastrophic cycle
when the rocks of the shear zone were thrust and intruded
by acid or intermediate igneous rocks.
12. 5. Titaniferous and vanadiferous magnetites:
The vanadiferous-titaniferous magnetite deposits are
associated with gabbroid and ultrabasic rocks.
In Karnataka titaneferous magnetites occur as linear
bands with prominent outcrops in a narrow belt of
Dharwar rocks which are composed of amphibolites
and hornblende schists surrounded by Peninsular
Gneisses and intruded by an ultrabasic complex.
13. 6. Fault and fissure filling deposits:
This type of deposits occur in a fault zone traversing
the gneisses and Cuddapah formation over a length of
several km.
The ore bodies form low hillocks or ridges which
stand out well above the ground and are lens-shaped;
they also form veins and stringers in the fault zone.
The ore is generally haematite and is often slightly
specular in character and also jaspery when it is
siliceous.
14. Distribution and occurrences:
The major deposits of iron ore are located in:
o Jharkhand,
o Orissa,
o Chattisgarh,
o Karnataka
o Maharshtra
o Andhra pradesh
o Goa
16. Formation Nature of ore Occurrence
Quaternary Laterite Many states derived from
many
formations including
Deccan Traps
Tertiary
Miocene & Eocene
Ironstone SouthIndia-Travancore,
Malabar etc.
Assam, NE states,
U.P.Kumaon
Gondwana
Barakar
Mahadeva
Triassic
Ironstones & shale
Ironstones & siderite
Siderite
Ironstones & siderite
Haematite & goethite
West Bengal (Birbhum)
Jharkhand-Auranga
coalfield
West Bengal –Raniganj
coalfield
Kashmir
Indian iron ore formation and occurrences:
21. The Rajhara Iron Mine of Durg disyrict in the Indian state of Chhattisgarh
22. Conclusion:
Iron has found its usage from a very early part of human
civilization, second only to copper-bronze.
Haematite and magnetite are the two important iron ores
from which iron is extracted.
Iron is widely in the construction of roads, railways, other
infrastructure, appliances, and buildings.
Iron ore deposits are aalmost found in every state.
However 96% of total reserves are in Orissaa, Jharkhand,
Chhattisgarh, Karnataka, Andhra Pradesh, Maharashtra
and Goa.
23. References:
S.Krishnaswamy (1979) India’s Mineral Resources, Oxford & IBH
Publishing Co., New Delhi, 2nd
Edition, page 257-284
B.P.Radhakrishna (1996) Mineral Resources of Karnataka, Geological
Society of India, Bangalore, page 285-323
Websites:
www.geology.com
http://en.wikipedia.org/wiki/Iron_ore
www.google.com
Detailed Information Dossier (DID) on iron ore in India, Geological
Survey of India, pdf