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.
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.
Minerals are formed by changes in chemical energy in systems which contain one fluid or vapor phase. In nature, minerals are formed by crystallisation or precipitation from concentrated solutions. These solutions are called as ore-bearing fluids. Ore-bearing fluids are characterised by high concentration of certain metallic or other elements.
Fluids are the most effective agents for the transport of material in the mantle and the Earth's crust.
A presentation on Hydrothermal wall rock alteration with case studies on geophysical applications.
References : https://drive.google.com/drive/folders/16VSZMPMASMNVB47JdBUa_7udBk1qvK2U?usp=sharing
It covers seismic method, gravity method, electromagnetic method, magnetic method and radiometric method. all these methods help in mineral exploration
Slides related to wall rock alteration.In these slides it is described that how host rock behave when it comes in contact with the hydro thermal fluid coming from deep Earth (Mantle) and their results.
CLASSIFICATION OF ORE DEPOSITS
The Mixture of ore minerals are gangue minerals form an Ore deposit. The ore
deposits are generally found enclosed within the country rocks. The ore deposits
are formed in many different ways. Depending upon the process that may
operate to produce them, the ore deposits may be classified as follow:
Magmatic ore deposits.
Sublimation ore deposits.
Pegmatitic ore deposits.
Contact metasomatic ore deposits.
Hydrothermal ore deposits
Cavity filling deposits.
Replacement deposits.
Sedimentation ore deposits.
Evaporation ore deposits.
Residual and mechanical concentration deposits
Metamorphic ore deposits.
MAGMATIC ORE DEPOSITS:
The magmatic ore deposits are the magmatic products which crystallize from
magmas. The magmatic ore deposits are classified as follows:
o Early magmatic deposits
o Late magmatic deposits
Early magmatic deposits:
Early magmatic deposits are formed during the
early stage of the magmatic period. In this case the
ore minerals crystallize earlier than the rock
silicates. The Minerals of Nickel, Chromium, and
Platinum are usually found as early magmatic
deposits. The early magmatic deposits can be sub
divided into two groups:
o Dissemination deposits
o Segregation deposits
Dissemination deposits:
When magma crystallizes
conditions, a granular igneous rock is formed. In
such a rock early formed crystals of
may occur in dissemination.
Segregation deposits:
Magmatic segregation deposits are
formed as a result of gravitative
crystallization differentiation. In
case, the ore mineral which crystallize
early, get ocean-trated on a particular
part of igneous part. The ore deposits
thus formed are known as “Segregation
deposits”.
rly under seated
ore minerals
such
Late Magmatic Deposits:
The ore deposits which are formed to
called late magmatic deposits. The late magmatic deposits contain those ore
minerals which have crystallized at rather low temperature from the residual
magma. The magma which is left after crystallization of early for
is called residual magma. This magma frequently contains many ore minerals. The
late magmatic deposits include most of the magmatic deposits of iron and
titanium ores, these deposits are almost always associated with mafic igneous
rocks.
SUBLIMATION DEPOSITS:
Sublimation is a very minor process of formation of ore deposits. Sublimation
deposits contain only those minerals which have been volatilized by hear and
subsequently redeposit in the same form at low temperature and pressure. The
sublimation deposits are found associated with Volcanoes and Fumaroles. Sulfur
of this origin has been mined in Japan, Italy, and Mexico.
Introduction of mineral deposits: Mineral deposit ; A geological definition of an ore deposit; Ore Deposit Environments; The significance of ore deposit size; Which commodities are included by the definition of Ore Deposits ; The extraction of an economic commodity from ore ; Geological Factors Affecting Economics of Ore Extraction ; Shape and depth of the deposit; Mineralogy and texture of the ore; The presence of multiple extractable products; Metals enrichment factors; Ore Deposit Constitutes; Ore Deposit Geology and Related Sciences; Structural Control Ore Deposits; Depth of Occurrence Mineral deposits; Nature of Mineralization; Morphology of Ore Deposit; Geographical Localization of Ore Deposits;
Orebodies; oreshoots; ore deposits; ore reserves
Minerals are formed by changes in chemical energy in systems which contain one fluid or vapor phase. In nature, minerals are formed by crystallisation or precipitation from concentrated solutions. These solutions are called as ore-bearing fluids. Ore-bearing fluids are characterised by high concentration of certain metallic or other elements.
Fluids are the most effective agents for the transport of material in the mantle and the Earth's crust.
A presentation on Hydrothermal wall rock alteration with case studies on geophysical applications.
References : https://drive.google.com/drive/folders/16VSZMPMASMNVB47JdBUa_7udBk1qvK2U?usp=sharing
It covers seismic method, gravity method, electromagnetic method, magnetic method and radiometric method. all these methods help in mineral exploration
Slides related to wall rock alteration.In these slides it is described that how host rock behave when it comes in contact with the hydro thermal fluid coming from deep Earth (Mantle) and their results.
CLASSIFICATION OF ORE DEPOSITS
The Mixture of ore minerals are gangue minerals form an Ore deposit. The ore
deposits are generally found enclosed within the country rocks. The ore deposits
are formed in many different ways. Depending upon the process that may
operate to produce them, the ore deposits may be classified as follow:
Magmatic ore deposits.
Sublimation ore deposits.
Pegmatitic ore deposits.
Contact metasomatic ore deposits.
Hydrothermal ore deposits
Cavity filling deposits.
Replacement deposits.
Sedimentation ore deposits.
Evaporation ore deposits.
Residual and mechanical concentration deposits
Metamorphic ore deposits.
MAGMATIC ORE DEPOSITS:
The magmatic ore deposits are the magmatic products which crystallize from
magmas. The magmatic ore deposits are classified as follows:
o Early magmatic deposits
o Late magmatic deposits
Early magmatic deposits:
Early magmatic deposits are formed during the
early stage of the magmatic period. In this case the
ore minerals crystallize earlier than the rock
silicates. The Minerals of Nickel, Chromium, and
Platinum are usually found as early magmatic
deposits. The early magmatic deposits can be sub
divided into two groups:
o Dissemination deposits
o Segregation deposits
Dissemination deposits:
When magma crystallizes
conditions, a granular igneous rock is formed. In
such a rock early formed crystals of
may occur in dissemination.
Segregation deposits:
Magmatic segregation deposits are
formed as a result of gravitative
crystallization differentiation. In
case, the ore mineral which crystallize
early, get ocean-trated on a particular
part of igneous part. The ore deposits
thus formed are known as “Segregation
deposits”.
rly under seated
ore minerals
such
Late Magmatic Deposits:
The ore deposits which are formed to
called late magmatic deposits. The late magmatic deposits contain those ore
minerals which have crystallized at rather low temperature from the residual
magma. The magma which is left after crystallization of early for
is called residual magma. This magma frequently contains many ore minerals. The
late magmatic deposits include most of the magmatic deposits of iron and
titanium ores, these deposits are almost always associated with mafic igneous
rocks.
SUBLIMATION DEPOSITS:
Sublimation is a very minor process of formation of ore deposits. Sublimation
deposits contain only those minerals which have been volatilized by hear and
subsequently redeposit in the same form at low temperature and pressure. The
sublimation deposits are found associated with Volcanoes and Fumaroles. Sulfur
of this origin has been mined in Japan, Italy, and Mexico.
Introduction of mineral deposits: Mineral deposit ; A geological definition of an ore deposit; Ore Deposit Environments; The significance of ore deposit size; Which commodities are included by the definition of Ore Deposits ; The extraction of an economic commodity from ore ; Geological Factors Affecting Economics of Ore Extraction ; Shape and depth of the deposit; Mineralogy and texture of the ore; The presence of multiple extractable products; Metals enrichment factors; Ore Deposit Constitutes; Ore Deposit Geology and Related Sciences; Structural Control Ore Deposits; Depth of Occurrence Mineral deposits; Nature of Mineralization; Morphology of Ore Deposit; Geographical Localization of Ore Deposits;
Orebodies; oreshoots; ore deposits; ore reserves
PetroSync - Surface Geochemical Exploration for Oil and GasPetroSync
The great majority of oil and gas pools and mature source rocks have recognizable surface geochemical expression. The O&G industry devotes significant time and resources in finding and defining traps, but little or none in establishing the likely presence of hydrocarbon in those traps, especially for older onshore basins.
On 9/10 March, MCRB hosted a multistakeholder discussion on licensing and responsible business practices for gold mining in Sagaing Region bringing together government officials from the Mining, Forestry and Environmental Conservation Departments of the Ministry of Natural Resources and Environmental Conservation (MONREC), General Administration Department (GAD), the Directorate of Investment and Companies Administration (DICA) and the Ministry of Agriculture, Livestock and Irrigation (MoALI), together with parliamentarians from across Sagaing Region, including Homalin, Tigyaing , Kawlin, Wuntho, Indaw, and Pinlebu townships. They were joined in Monywa by local and international mining companies, civil society organisations and international NGOs and experts.
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This was the presentation of design project 1 (PGE 405).A project about Improved reservoir Evaluation. In this project, I discussed using different techniques in reservoir evaluation as well as using downhole fluid analysis.
Methods and stages of Mineral Exploration: Adaptive Resource Management PlanNgatcha Bryan
Exploration can be divided into a number of interlinked and sequential stages which involve increasing
expenditure and decreasing risk. Early stages of exploration are planning and prospecting. The planning
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exploration entity. Prospecting covers activities leading to the selection of an area for detailed ground
work; this is the point at which land is acquired. The subsequent stages involve targeted prospecting and
exploration in order to quantify and qualify the mineral resources. Pre-feasibility study is then
performed for evaluating the commercial viability of the deposit (Adapted from Moon et al., 2006).
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2. CONTENTS
INTRODUCTION
GENERAL PRINCIPLES
OPTIMIZATION OF EXPLORATION
PLANNING OF EXPLORATION
SELECTION OF PROFESSIONAL LEADERSHIP
SELECTION OF AREAS
THE EXPLORATION SEQUENCE
CHOICE OF EXPLORATION METHODS
TARGET SIZE
PROPETRY CONTROL
RELIABILITY OF METHOD
COST
VALUE OF EXPECTED ORE
THE ROLE OF GEOCHEMISTRY
ORGANISATION AND OPERATIONS
Field operation
Laboratory
Supervision
CONCLUSION
REFERENCE
3. INTRODUCTION
oGeochemical prospecting for minerals includes any
method of mineral exploration based upon systematic
measurement of one or more chemical properties of a
naturally occurring material.
oThe chemical property measured is most commonly the
trace content of some element or group of elements.
o The naturally occurring material may be rock, soil,
gossan,glacial debris, vegetation, stream sediment, or
water.
oThe purpose of the measurements is the discovery of a
geochemical "anomaly" or area where the chemical
pattern indicates the presence of ore in the vicinity.
4. GENERAL PRINCIPLES OF
GEOCHEMISTRY
Mineral deposits represent anomalous concentrations of
specific elements, usually within a relatively confined
volume of the Earth's crust.
Most mineral deposits include a central zone, or core, in
which the valuable elements or minerals are
concentrated.
This zone surrounding the core deposit is known as a
primary halo or anomaly.
5. OPTIMIZATION OF EXPLORATION
Any exploration requires an immediate outlay of
money and time, with the hope that discovery and
exploitation of an ore body in the future will more
than repay the initial cost.
At the initiation of a typical exploration project , the
probability of success on the project is very small.
The total costs must include not only those for the
reconnaissance survey and any successful detailed
surveys.
7. SELECTION OF PROFESSIONAL LEADERSHIP
• Many exploration surveys have fallen short of expectations
through lack of experience and technical training.
• More often it is necessary to build up a team ,the member
of which cooperate to provide the necessary virtues.
• The critical phases of orientation, planning and
interpretations can be done by professional exploration
geologists or geochemists.
8. SELECTION OF AREAS
The main purpose of this stage is to select areas or regions
that have good mineral potential and that can be
prospected effectively.
Initial selection of areas should be based on a most
through review of the known geology and records of past
mining and prospecting activity.
Based on recorded mineralization and on the geological
environment.
9. THE EXPLORATION SEQUENCE
o A large exploration program is commonly organized as a
logical sequence of operations.
o Each stage in this sequence involves the study of
methods in most effective.
o At the end of the each stage ,the available information is
evaluated and used to select smaller areas for detailed
study ,or to terminate the program if the initial premises
have been disproved.
10. CHOICE OF EXPLORATION METHODS
o For greatest overall effectiveness, an optimum balance
must be struck between the various geological ,
geophysical , and geochemical methods that are known
to be applicable.
o The choice must be based on relevant previous
experience and case-history data.
o Selection of methods is also strongly influenced by the
size of the target and by property control.
11. TARGET SIZE
Some features of ore environment, such as favorable
host rocks ,geological structures , or geochemical
provinces , are related to the genesis and localization.
Each geological , geophysical ,and geochemical features
of the ore environment defines a target area of
characteristic size , shape ,and relationship to the ore.
12. PROPETRY CONTROL
The acquisition of property rights ,in most countries ,is an
extremely tedious and expensive phase of mineral
exploration.
The general pattern of exploration may be modified or
even dominated by property consideration.
13. RELIABILITY OF METHOD
Reliability depends not only on how effective the
exploration method is in locating the target , but also
extent to which an anomaly is specifically related to ore
and the abundance of non-significance anomalies that
may confuse interpretation and require fallow-up survey.
COST
The cost of an exploration survey is the only one of the
critical factor that can be estimated with any degree of
accuracy.
14. VALUE OF EXPECTED ORE
The expected value of the ore body being sought and
the chances of success may have an appreciable
bearing on the applicability of a given method.
Thus a high-cost survey is justified for large ore bodies
are expected and there is relatively little chances of
overlooking a deposit.
Conversely , a low cost-survey is justified in areas of
small targets.
15. THE ROLE OF GEOCHEMISTRY IN AN
EXPLORATION SYSTEM
Geochemistry is an essential component in most modern
integrated mineral exploration programs, for the following
reasons:-
(1) Economic mineral deposits are commonly characterized
by their low grade and large tonnage. Discovery, assessment
and development are highly dependent upon geochemical
methods and analyses.
(2) Exploration activity is mostly carried out in tropical and
subtropical environments where chemical weathering has
predominated and where geochemical prospecting techniques
have proven most effective.
Recent estimates suggest that between 10 and 25% of
exploration budgets are allocated to geochemistry.
16. ORGANISATION AND OPERATIONS
Every geochemical survey organization ,
irrespective of it’s scale, is based on three main
functional units :
Field operation
Laboratory
Supervision
17. FIELD OPERATION
Most operation in a
systematic sampling
program can be carried out
by team of local workers
under the supervision of
trained field assistants.
18. LABORATORY
In general ,most efficient
,reliable ,and economical
analytical work is done in
an established laboratory.
In many laboratories ,
sample preparation and
analysis is performed by
locally recruited labor.
19. SUPERVISION
Geochemical surveys should always be the
responsibility of one who is first experienced
exploration geologist.
His responsibilities will include :
(1) Orientation to establish both field and laboratory
techniques.
(2) Maintenance of technical efficiency and
coordinate throughout the operation.
20. CONCLUSION
Geochemical methods of exploration constitutes an
important tool in the investigation of the economic
mineral deposits.
Any geochemical investigation to be effective, must
take into consideration several aspects of the ore
body, including genesis and cost at various stages
of exploration.
21. REFERENCE
H. E. Hawkes and J. S. Webb (1979) Geochemistry
in mineral exploration ,second edition ,Pp:535-548.
www.wekipedia.com