Sedimentary basins are the depressions in the earth's crust where loose particles accumulate and finally lithified to form sedimentary rocks. Basins are particularly attractive to geoscientists from time immemorial due to the wealth hidden here in the form of oil, gas, coal etc. In this document you will find the types of basins, basin-fill types, methods of basin analysis and so on.
What is an ore?, Ore deposit environments, Formation of Mineral Deposits, Endogenous (Internal) processes, Exogenous (Surficial) processes, Types of Sedimentary Rocks, Mineral Deposits Associated with Sedimentary Process, physical processes of ore deposit formation in the surficial realm, Erosion, weathering , transportation, sorting, Precipitation, Depositional Environments, Deposits formed by Weathering, Deposits formed by Sediment, Resources from the Sedimentary Environments
Sedimentary basins are the depressions in the earth's crust where loose particles accumulate and finally lithified to form sedimentary rocks. Basins are particularly attractive to geoscientists from time immemorial due to the wealth hidden here in the form of oil, gas, coal etc. In this document you will find the types of basins, basin-fill types, methods of basin analysis and so on.
What is an ore?, Ore deposit environments, Formation of Mineral Deposits, Endogenous (Internal) processes, Exogenous (Surficial) processes, Types of Sedimentary Rocks, Mineral Deposits Associated with Sedimentary Process, physical processes of ore deposit formation in the surficial realm, Erosion, weathering , transportation, sorting, Precipitation, Depositional Environments, Deposits formed by Weathering, Deposits formed by Sediment, Resources from the Sedimentary Environments
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
HYDROTHERMAL PROCESSES; Causes of deposition; Origin of Hydrothermal Fluids (or The Main Sources of Water in Hydrothermal System); The Main Steps in Hydrothermal Processes; Classification of Hydrothermal Deposits; Different Types of Hydrothermal Vein; Different styles of Hydrothermal ore deposits; Orogenic Hydrothermal Ore Deposits; Hypozonal: Orogenic, hydrothermal ore deposits; Epizonal:; Mesozonal
A presentation on Hydrothermal wall rock alteration with case studies on geophysical applications.
References : https://drive.google.com/drive/folders/16VSZMPMASMNVB47JdBUa_7udBk1qvK2U?usp=sharing
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.
Texture of Ore Minerals; Importance of Studying Textures; Individual Grains Properties; Filling of voids; Texture Types; Genetically differentiated between Texture types; Secondary textures from replacement; Hypogene Texture; Supergene Texture; Primary texture formed from Melts; Primary texture of open-space deposition; Secondary textures from cooling; Secondary textures from deformation; TEXTURES OF ECONOMIC ORE DEPOSITS; Textures of Magmatic ores; Cumulus textures; Intergranular or intercumulus textures; Exsolution textures; Textures of hydrothermal ore deposits and skarns; Replacement textures; Open space filling textures; Textures characteristic of surfacial or near surface environments and processes; Criteria for identifying replacement textures; Vein and Veining have different Nature Features
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.
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.
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
HYDROTHERMAL PROCESSES; Causes of deposition; Origin of Hydrothermal Fluids (or The Main Sources of Water in Hydrothermal System); The Main Steps in Hydrothermal Processes; Classification of Hydrothermal Deposits; Different Types of Hydrothermal Vein; Different styles of Hydrothermal ore deposits; Orogenic Hydrothermal Ore Deposits; Hypozonal: Orogenic, hydrothermal ore deposits; Epizonal:; Mesozonal
A presentation on Hydrothermal wall rock alteration with case studies on geophysical applications.
References : https://drive.google.com/drive/folders/16VSZMPMASMNVB47JdBUa_7udBk1qvK2U?usp=sharing
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.
Texture of Ore Minerals; Importance of Studying Textures; Individual Grains Properties; Filling of voids; Texture Types; Genetically differentiated between Texture types; Secondary textures from replacement; Hypogene Texture; Supergene Texture; Primary texture formed from Melts; Primary texture of open-space deposition; Secondary textures from cooling; Secondary textures from deformation; TEXTURES OF ECONOMIC ORE DEPOSITS; Textures of Magmatic ores; Cumulus textures; Intergranular or intercumulus textures; Exsolution textures; Textures of hydrothermal ore deposits and skarns; Replacement textures; Open space filling textures; Textures characteristic of surfacial or near surface environments and processes; Criteria for identifying replacement textures; Vein and Veining have different Nature Features
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.
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.
This is the presentation about the Geothermal energy evolving in the world. It describes about different technology and use of it. It is beneficial for students to present this topic in their academic institutions. Also they will get brief knowledge about the geothermal energy from renewable energy.
Solution Mining; Technology of the Salt Production; Rock salt (NaCl); Sylvinite; Solution mining of carnallitite with; two wells; selective dissolution; hot leaching; Methods to control the size of the caverns; INTRODUCTION; TECHNOLOGY OF SOLUTION MINING; FRASCH PROCESS-SULFUR PRODUCTION; TECHNOLOGY OF THE SALT PRODUCTION; What is Rock salt ?; Evaporite deposits ; Rock salt; Sylvinite; Carnallite; HEAP LEACHING; Heap leach production model; Important parameters during metallurgical testing; Staged Approach to Heap Leach Testwork and Design; Uranium Heap Leaching; Uranium Ore Minerals; Basic Geochemistry of Uranium Minerals; Copper Heap Leaching; Layout of copper bio-heap pilot plant; Laterite heap leaching; Nickel Laterite Deposits; Proposed counter-current heap leach arrangement; Neutralizing potential of laterites in 6 meter column; Advantages and Problems of Solution Mining
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.
The Art Pastor's Guide to Sabbath | Steve ThomasonSteve Thomason
What is the purpose of the Sabbath Law in the Torah. It is interesting to compare how the context of the law shifts from Exodus to Deuteronomy. Who gets to rest, and why?
We all have good and bad thoughts from time to time and situation to situation. We are bombarded daily with spiraling thoughts(both negative and positive) creating all-consuming feel , making us difficult to manage with associated suffering. Good thoughts are like our Mob Signal (Positive thought) amidst noise(negative thought) in the atmosphere. Negative thoughts like noise outweigh positive thoughts. These thoughts often create unwanted confusion, trouble, stress and frustration in our mind as well as chaos in our physical world. Negative thoughts are also known as “distorted thinking”.
The Roman Empire A Historical Colossus.pdfkaushalkr1407
The Roman Empire, a vast and enduring power, stands as one of history's most remarkable civilizations, leaving an indelible imprint on the world. It emerged from the Roman Republic, transitioning into an imperial powerhouse under the leadership of Augustus Caesar in 27 BCE. This transformation marked the beginning of an era defined by unprecedented territorial expansion, architectural marvels, and profound cultural influence.
The empire's roots lie in the city of Rome, founded, according to legend, by Romulus in 753 BCE. Over centuries, Rome evolved from a small settlement to a formidable republic, characterized by a complex political system with elected officials and checks on power. However, internal strife, class conflicts, and military ambitions paved the way for the end of the Republic. Julius Caesar’s dictatorship and subsequent assassination in 44 BCE created a power vacuum, leading to a civil war. Octavian, later Augustus, emerged victorious, heralding the Roman Empire’s birth.
Under Augustus, the empire experienced the Pax Romana, a 200-year period of relative peace and stability. Augustus reformed the military, established efficient administrative systems, and initiated grand construction projects. The empire's borders expanded, encompassing territories from Britain to Egypt and from Spain to the Euphrates. Roman legions, renowned for their discipline and engineering prowess, secured and maintained these vast territories, building roads, fortifications, and cities that facilitated control and integration.
The Roman Empire’s society was hierarchical, with a rigid class system. At the top were the patricians, wealthy elites who held significant political power. Below them were the plebeians, free citizens with limited political influence, and the vast numbers of slaves who formed the backbone of the economy. The family unit was central, governed by the paterfamilias, the male head who held absolute authority.
Culturally, the Romans were eclectic, absorbing and adapting elements from the civilizations they encountered, particularly the Greeks. Roman art, literature, and philosophy reflected this synthesis, creating a rich cultural tapestry. Latin, the Roman language, became the lingua franca of the Western world, influencing numerous modern languages.
Roman architecture and engineering achievements were monumental. They perfected the arch, vault, and dome, constructing enduring structures like the Colosseum, Pantheon, and aqueducts. These engineering marvels not only showcased Roman ingenuity but also served practical purposes, from public entertainment to water supply.
How to Create Map Views in the Odoo 17 ERPCeline George
The map views are useful for providing a geographical representation of data. They allow users to visualize and analyze the data in a more intuitive manner.
Instructions for Submissions thorugh G- Classroom.pptxJheel Barad
This presentation provides a briefing on how to upload submissions and documents in Google Classroom. It was prepared as part of an orientation for new Sainik School in-service teacher trainees. As a training officer, my goal is to ensure that you are comfortable and proficient with this essential tool for managing assignments and fostering student engagement.
7. Plate tectonics & Metamorphism in
the HYDROTHERMAL PROCESS
• Hydrothermal Activity at Divergent Plate
Boundaries
• Metasomatism
• Hydrothermal Rocks and Minerals
• Sources of Water
10. Hydrothermal Ore Bodies
• 600 C: Tungsten , Tin in Granites
• 400 C: Gold, Uranium , Silver , Cobalt , Molybdenum,
Copper
– Gold-Quartz deposits
– Porphyry Copper
– Marginal ores around intrusions
• 200 C: Copper, Zinc, Cadmium, lead
– Outer contact zones
– Mississippi Valley ore deposits
• Cool: Mercury, Arsenic
– Hot springs, fault zones
11. HYDROTHERMAL ORE DEPOSITS
DEPTH-TEMPERATURE CLASSIFICATION
I) Epithermal deposits
shallow depth of formation and moderate
temperature
II) Meso-thermal deposits
moderate depth of formation and temperature
III) Hypothermal deposits
great depth of formation and temperature
IV) High level, high temperature intrusion-related
deposits
porphyry and skarn deposits
12.
13. A hydrothermal vent is a
fissure in a planet's surface
from which exothermally
heated water issues.
Hydrothermal vents are
commonly found near
volcanically active places,
areas where tectonic
plates are moving apart,
ocean basins, and
hotspots.
14. A Sea Vent
• Is a type of hydrothermal vent found on the ocean
floor.
• Formed in fields hundreds of meters wide when
superheated water from below Earth's crust comes
through the ocean floor.
• This water is rich in dissolved minerals from the crust,
most notably sulfides. When it comes in contact with
cold ocean water, many minerals precipitate, forming a
black chimney-like structure around each vent.
• The metal sulfides that are deposited can become
massive sulfide ore deposits in time.
15. • What appears to be black smoke exiting the
vent is actually a highly concentrated mineral
and metal cocktail drawn from the center of
the Earth itself.
• When these materials hit the frigid waters of
the deep sea, they precipitate out of the fluid
and rain down upon the seabed below.
16. • Is a type of hydrothermal vent found on the
ocean floor.
• Formed in fields hundreds of meters wide when
superheated water from below Earth's crust
comes through the ocean floor.
• Is rich in dissolved minerals from the crust, most
notably sulfides.
• Many minerals precipitate, forming a black
chimney-like structure around each vent. The
metal sulfides that are deposited can become
massive sulfide ore deposits in time.
18. Vent as a SOURCE OF MINERAL
The materials contained in the vent fluid
includes iron, gold, silver, copper, zinc,
cadmium, manganese, and sulfur, along with
significant amounts of methane gas mixed
into the fluid.
Halides, sulphates, chromates, molybdates
and tungstates are also abundant.
19. Hydrothermal Fluids
• Hydrothermal fluid exits the vent system from
between 330C to 380C, can have a PH of around
2.4, and is generally found at very deep locations
(7000 or so feet).
• To keep the metallic sulfides in the solution, you
need to keep two things constant: temperature
and pressure. Hydrostatic pressure at those
depths is what keeps the water from turning into
steam as soon as it exits the vent. Mixing with
cold sea water (2-4C) is what causes
precipitation.
20. Recovery
While several additional stages of purification
will surely be necessary, the natural heat from
the process itself provides the most important
part of the energy needed for the process.
If only 50% of the total volume could be
recovered, that would still provide about a
billion liters, or 264,000,000 gallons of fresh
water daily.
21. FIRST ATTEMPT…
The Marshall Hydrothermal Recovery System brings
massive quantities of hydrothermal fluid to the surface.
Temperature is incredibly high, but it does not boil
because of the intense pressures at the depths where
the vents are located.
The volumes noted show about 76,000,000 liters, or
20,000,000 gallons of fluid brought to the surface every
hour.
As it rises through the insulated pipe structure and the
ambient pressure decreases, it will flash to steam,
which can be distilled back into fresh water.
22. Technology Involved…
• Uses a deceptively simple system of insulated
pipes and a funnel.
• No attempt to deal with the superheated
hydrothermal fluid at the bottom of the
ocean.
• Ducting that fluid to the surface to be
processed on platforms similar to those used
for oil exploration and drilling.
23. FLUID INVOLVED
Fluid is trapped when it is hot and is
maintained within an insulated structure,
which stays hot and rise.
Moves through the pipe by a combination
of vent flow velocity, convection, conduction,
and flash steam pressure generated as the
superheated fluid rises and the ambient
pressure diminishes.
A funnel mouth at the input end would act
as a venturi to increase flow velocity within
the pipe.
26. Base is of highly stable circles and triangles.
The first section of pipe at the top of the cone is the
one that takes the weight of the column of pipe to
be built above.
The intake pipe is placed as deep down into the vent
as possible, to recover the highest temperature fluid.
Anchors can be drilled through the bottom ring and
into the seabed below for additional stability.
The funnel at the intake end is designed to act like a
venturi to increase the velocity of the fluid within the
pipe.
Weight was an issue.
A further source of concern was vertical stability.
27. The fluid would be utilized at the surface by
providing the heat for traditional steam turbine
generation.
The superheated fluid would either be used
directly or it could heat a clean working fluid within
a heat exchanger to ultimately drive the turbines.
On the Juan de Fuca Ridge for example,
which lies about 200 miles off the coast of
Seattle, the main active vent field is about 180 m
wide and 350 m long.
28. STABILITY OF THE RIG
Buoyancy collars were added to the design.
The vertical stability would be greatly enhanced.
Adding in swiveling connections between the pipe
segments to allow flexibility and using intermittent
mooring lines to stabilize the column were the
finishing touches.
29. The complete Hydrothermal Recovery System, showing electric generation,
water desalination, and mining facilities operating together.
30. Extracting metals directly from
hydrothermal fluids
The idea is to pump the fluid directly into
some kind of metal extraction process before
the sulfides can precipitate.
31. CASE STUDIES
• In 2005, Neptune Resources , was granted
35,000 km² of exploration rights over the
Kermadec Arc in New Zealand's Exclusive
Economic Zone to explore for seafloor massive
sulfide deposits, a potential new source of lead-
zinc-copper sulfides formed from modern
hydrothermal vent fields.
• An April 2007 exploration of the deep-sea vents
off the coast of Fiji found those vents to be a
significant source of dissolved iron.
33. PROBLEMS ASSOCIATED…
• Very high temp. of the fluid.
• Keeping the minerals in solution while
pumping it through pipes.
• If any minerals precipitate in the pipes, it'll
plug up the whole system.
34. REMEDIES…
• Pumping solutions with precipitates doesn't
sound very good - why not filter off the solids?
• Alternatively, could we just pump large
amounts of acid down and dissolve the
metals.
35. TO SUM UP…
• Lot of good metals are dissolved in hydrothermal
vent fluids.
• Metals come out of solution when the water
cools.
• They precipitate out. They fall on the ocean floor.
• Just go down to the sites of dead smokers
(where all the life has died off) and scrape up the
ocean floor by some dredging arrangement!
36. • Set up structures near the smokers composed of
metals .
• Desired substance would tend to precipitate out on it
or react with it. You could haul these things to the
surface like a lobster trap, scrape off all the thorium or
whatever, the drop it back down to pick up another
load.
• Some geothermal power plants have the problem that
they wash a lot of toxic metal compounds to the
surface. If you combine metal recovery with
geothermal power generation you may reach break
even earlier.
37. OTHER CONCERNS…
• At some depth (unknown at this time), hydrostatic pressure
would be insufficient to keep the hot fluid in a liquid state.
Beneath this point, a pump of some kind would need to be
installed to keep the fluid above it higher than the
threashold pressure. Pressure problem solved.
• At one point, it is considered depleated uranium as a
possible material to line the inside of the pipe with.
Unfortunatly, there are a host of environmental and
corrosion concerns with using this material.
• The technology for using titanium in this kind of application
already exists but hasn't been used in this application.
Corrosion problem likely solved.
38. Ecological Concerns…
• There is always a concern about the
environmental consequences that its
implementation might produce.
• Hydrothermal vents are home to an amazing
variety of organisms and animals that are
found nowhere else on Earth.
39. ADVANTAGES
• Driven by the elevated price activity in the
base metals sector.
• Extraction of mineral resources from
hydrothermal fields on the seafloor.
• Significant cost reductions are(in theory)
possible.
• Is a continuous process.
• Automation possible.
40. DEMERITS
• High initial Capital requirement.
• Adverse effects on marine organisms evident.
• Dependence on oceanic currents.
• Less know-how known.
41. PRESENT FACILITIES ROUND THE
GLOBE
• Nautilus Minerals :
Advanced stages of commencing extraction from
its Solwarra deposit, in the Bismarck Archipelago
• Neptune Minerals is at an earlier stage with its
Rumble II West deposit, located on the Kermadec
Arc, near the Kermadec Islands.
• Nautilus Minerals, in partnership with Placer
Dome (now part of Barrick Gold), succeeded in
2006 in returning over 10 tones of mined SMS to
the surface using modified drum cutters mounted
on an ROV - a world first.