This presentation discusses heavy minerals, which have a density over 2.8g/cm3 and comprise less than 1% of sandstone. Heavy minerals can be extracted via dry mining of shallow deposits or wet mining using dredges for deeper deposits below the water table. Seventeen placer deposits of heavy minerals have been found along the coast of Bangladesh, containing over 4 million tons of minerals like ilmenite, magnetite, zircon, and rutile. These heavy mineral deposits represent an important economic resource for Bangladesh.
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.
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.
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.
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.
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
The name ophiolite derived from Greek root which means
Ophio : snake or serpent Litho : Stone
The green colour, structure and texture of sheared ultramafic rocks is similar to some serpents
Economically :
Massive Sulphide
It founded within pillow lava most of massive Sulphide associated in ophiolites have well developed Gossans (bright colored iron oxide, hydroxides, and sulfides) which is very rich in gold.
Chromite
Stratiform (be tabular or pencil shape) or podiform (irregular shape) within ultra-mafic rocks
These deposits are developed on serpentinite peridotite
Laterites (nickel and iron)
Asbestos
Talc
Magenesite
ophiolite sequence :
Sediments
Pillow Lavas
Dykes
Gabbros
Layered Gabbro
Layered Peridotite
Upper mantle
Boundary problems between :-
Precambrian/Cambrian
Permian/Triassic
Cretaceous/Tertiary
Neogene/Quaternary
Stratigraphic boundaries are determined by one or more of geological events such as volcanic activity, sedimentation, tectonism, paleo-environments & evolution of life.
Faunal records have played major role in determining the boundaries of the Phanerozoic units.
The other geological events are dated on the evidence of fossil records.
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
The name ophiolite derived from Greek root which means
Ophio : snake or serpent Litho : Stone
The green colour, structure and texture of sheared ultramafic rocks is similar to some serpents
Economically :
Massive Sulphide
It founded within pillow lava most of massive Sulphide associated in ophiolites have well developed Gossans (bright colored iron oxide, hydroxides, and sulfides) which is very rich in gold.
Chromite
Stratiform (be tabular or pencil shape) or podiform (irregular shape) within ultra-mafic rocks
These deposits are developed on serpentinite peridotite
Laterites (nickel and iron)
Asbestos
Talc
Magenesite
ophiolite sequence :
Sediments
Pillow Lavas
Dykes
Gabbros
Layered Gabbro
Layered Peridotite
Upper mantle
Boundary problems between :-
Precambrian/Cambrian
Permian/Triassic
Cretaceous/Tertiary
Neogene/Quaternary
Stratigraphic boundaries are determined by one or more of geological events such as volcanic activity, sedimentation, tectonism, paleo-environments & evolution of life.
Faunal records have played major role in determining the boundaries of the Phanerozoic units.
The other geological events are dated on the evidence of fossil records.
Deep sea mining is a new frontier for mining engineers. Sea floor holds the potential mineral that are vital for development which is not even explored, the advancement of technology in the time will enable to access reliable infrastructure and methods to extract sea floor without compromising the sustainability and eco friendly.
Heavy Mineral Studies of Beach Sands of Vagathor, North Goa, IndiaIJMER
Vagator beach is situated 22 km away from panjim on the northern side Bardez taluk
approachable via Candolim are Mapusa by road. The beach is projected on both the sides by
promontories. The beach is in arcuate shape, the area included with survey of India toposheet No
48/E/14 which is bounded by latitudes 15º35ˈN 15º38ˈN and longitude 78º43ˈE. The Chapora river
and its tributaries drain the entire region that is the Vagator beach. It flows from North-East to
South-West direction. The drainage pattern is structurally controlled; the Chapora River has its
source in the Ramghat hills of Belgaum district in Karnataka then it flows through the Thilari ghat
and enters Goa. Its length in Goa is about 31 km and the mouth of the river bank, mud bank and
mangroves swamps are common.
In laboratory techniques heavy mineral separation are based mass separation in a liquid
with specific gravity and magnetic separation using hand magnet and Frantz isodynamic separator
at different volts. X-ray analysis was carried out by using RIGAKU ALTIMA IV copper target on the
basis of Bragg’s law. The non magnetic sand grains was observed under optical microscope to
identify diagnostic properties of minerals.
The heavy mineral shoot comprises of opaque (magnetite and illmenite) and transparent heavy
minerals like hornblende, epidote, garnet, rutile, zircon, enstatite and minor amounts of tourmaline.
The light minerals are mainly quartz and feldspars. The magnetite concentration ranges between 2.01
to 56.86% and Ilmenite between 2.83 to 41.04% and non mangnetics between 1.18 to 44.81%. X ray
diffraction studies and SEM (Scanning electron microscope) studies were employed to study the
mineralogical composition of beach sands of Vagator and detailed investigations are dealt in the
paper.
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Ore Minerals (How it is found, mined, and processed for human use)Simple ABbieC
Department of Education | Senior High School
Topic: Ore Minerals (How it is found, mined, and processed for human use)
Learning Competency:
Earth Science (for STEM): Describe how ore minerals are found, mined, and processed for human use. (S11ES-Ic-d-8)
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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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Prepare a presentation or a paper using research, basic comparative analysis, data organization and application of economic information. You will make an informed assessment of an economic climate outside of the United States to accomplish an entertainment industry objective.
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This Gasta posits a strategic approach to integrating AI into HEIs to prepare staff, students and the curriculum for an evolving world and workplace. We will highlight the advantages of working with these technologies beyond the realm of teaching, learning and assessment by considering prompt engineering skills, industry impact, curriculum changes, and the need for staff upskilling. In contrast, not engaging strategically with Generative AI poses risks, including falling behind peers, missed opportunities and failing to ensure our graduates remain employable. The rapid evolution of AI technologies necessitates a proactive and strategic approach if we are to remain relevant.
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4. Mineral
A mineral is a naturally occurring solid chemical
substance formed through bio- geochemical
processes, heaving characteristics chemical
composition, highly ordered atomic structure and
specific physical properties.
A mineral is an element or a chemical compound
that is normally crystalline and that has been
formed as a result of geological processes.
5.
6. Heavy Minerals
Heavy minerals have density of > 2.8gcm-3
and
typically comprise less than 1% of a sandstone. They
are more provenance specific than the light mineral
fraction .
Mineral sands contain suites of minerals with high
specific gravity known as heavy minerals.
7.
8. Furthermore, a distinction is made in the references
according to the density of the useable
heavy minerals:
• the heavy heavy minerals with a density of 6.8-21 g/cm3
(mainly gold, platinum, cassiterite),
• the light heavy minerals with a density of 4.2-6.7 g/cm3
(mainly ilmenite, rutile, zircon,
monazite, magnetite, chromite),
• gemstones with a density of 2.9-4.1 g/cm3 (mainly
diamond).
9.
10. Different types of minerals
Minerals are natural compounds formed through
geological process.
Minerals are needed by the body in small amounts to
help its function properly and strong.
There are two types of minerals :
Macro Mineral
Trace Mineral
11.
12.
13. Macro Mineral
Macro means “large” in Greek are dietary minerals
needed by the human body in high quantities. The
macro mineral group is made of calcium, phosphorus,
magnesium, sodium, potassium, chloride, sulfur.
14.
15.
16. Micro/Trace Mineral
Trace elements are micronutrients that are chemical
elements. A trace of something means that there is
only a little of it. So even though our body needs
mineral each day in small amounts for good health.
Trace minerals include iron, manganese, copper,
iodine, zinc, fluoride and selenium.
17.
18.
19. Heavy Mineral Extraction
Mining is the process of extracting valuable minerals
or other geological minerals form the earth crust.
Mining in broad sense means extracting of non-
renewable resources water petroleum and natural gas.
Mineral sands mining involves both dry mining and
wet (dredge) mining operation.
20. Heavy Mineral Extraction
The proper extraction processes for heavy minerals depend on
the depth of the groundwater
level, the degree of consolidation of the sediment and its
particle size. If the groundwater level is
sufficiently high and the sediment finely grained, extraction is
mostly economic if large-scale cutter
wheels or cutter head suction dredges that mechanically break
up solidified horizons are used. In
the case of very high extraction banks, the ore sand can be
pushed towards the suction dredger ship
using bulldozers. When gravel and stones are involved (e.g. gold
extraction in Alaska, cassiterite
extraction in South East Asia) floating bucket wheel dredges
are used. If the groundwater level is
very low, scraper bulldozers are used.
21.
22. Dry Mining Process
Dry mining typically involving the extraction of heavy
mineral ore from relatively shallow, unconsolidated,
and free flowing deposits. Dry mining is suitable
where deposits are shallow, contain hard brands of
rock or in a series of unconnected ore bodies.
23.
24.
25. Wet Mining Process
Dredge or wet mining is the best suited to ore
reservoir below the water table. Dredge mine is
artificial ponds, pumping ore in slurry form to a
floating concentrator. The ore is washed through
spirals that use specific gravity to separate the heavy
minerals sands from the lighter quartz and clay.
26.
27.
28. Transportation Deposition Of
Heavy Minerals
The heavy mineral became concentration into a
thin layer, composed of nearly 100% heavy
mineral, is known as heavy infra layer.
Lying beneath a thin surgical layer of low density
sediment is known as light supra layer.
Heavy mineral transported on the upper surface
of the heavy infra layer only when the local and
temporary erosion of light supra layer caused by
large clasts, clast jems or downstream moving
dune like bed forms exposed the heavy infra layer.
29.
30. History of HEAVY MINERALS In Bangladesh
Investigation of radioactive minerals like
MONAZITE by the erstwhile Geological Survey of
Pakistan around the cox’s bazaar sea beach area
started in 1961 and a number of precious heavy
minerals were identified the same year.
After systematic surveys during 1967 to 1969 it was
recognized that a potential zone of heavy mineral
exists along the entire coastal belt, mainly from
cox’s bazaar to badarmokam, and some areas of
maheskhali, kutubdia, and matabari island.
31. Later in 1975 a pilot plan was installed at katali,
cox’s bazaar with the cooperation of the Australian
Government.
By 1985 the nearly 550 km-long coastline of was
surveyed either partially or completely to map the
beach sand heavy minerals.
It was found that the reserves were concentrated
mainly along the sea beaches of chittagong & cox’s
bazaar districts .
32.
33. Present situation of HEAVY MINERALS
in Bangladesh
Untill now 17th
placer deposits are found ; 15th
are in
the cox’s bazaar, ctg. Sea beaches and nearby
offshore islands.
In fact seven are from cox’s bazaar – teknaf sea
beaches.
seven form Maheskhali Island, one each from
Matarbari, Kutubdia, Nijhum Island and Kuakata.
All the seventeen deposits include 20.5 million tons
of raw sand, which contains 4.4 millions of heavy
minerals.
34. Only eight types of economically important heavy
minerals, Namely
●Ilmenite , Magnetite, Zircon, Rutile, Garnet,● ● ● ● ●
Leucoxene, kyanite and monazite occur in these● ●
deposits .
The total stock of these eight types of heavy minerals
these seventeen deposits is 1761000 tons.
35.
36. submitted by : shuvo das
id no : 14207101
Email: shuvo.das.imsf@gmail.com