Mineral Deposit Geology and Models Flashcards

(37 cards)

1
Q

_____ which occurs at the surface can be worked by cheap open pit methods.

A

Large, low-grade deposits

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2
Q

_____ will necessitate more expensive underground methods of extraction

A

Thin tabular vein deposits

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3
Q

_____, aided by the savings from bulk handling of large daily tonnages, has led to a trend towards the large scale mining of low grade orebodies

A

Open pitting

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4
Q

Ore bodies of _____ can be mined more cheaply than those of _____, particularly when they include barren zones

A

regular shape, irregular shape

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5
Q

For an open pit mine, the shape and attitude of an orebody will also determine ____

A

how much waste has to be removed during mining

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6
Q

if an orebody viewed in plan is longer in one direction than the other, we can designate this long dimension as its _____.

A

strike

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7
Q

The inclination of the orebody perpendicular to the strike.

A

dip

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8
Q

The longest dimension of the orebody.

A

axis

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9
Q

The _____ of the axis is measured in the vertical
plane ABC

A

plunge

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10
Q

Can be measured in any other plane, the usual choice being the plane containing the strike,

A

pitch or rake

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11
Q

if the orebody is fault-controlled then the _____ may be measured in the fault plane.

A

pitch

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12
Q

These bodies are extensive in two dimensions but have restricted development in their third dimension.

A

Tabular orebodies

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13
Q

Frequently pinch and swell out as they are followed up or down a stratigraphical sequence

A

Vein

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14
Q

Sometimes called fissure-veins

A

Veins

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15
Q

Can create difficulties during both exploration and mining often because only the swells are workable.

A

pitch-and-swell structure

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16
Q

Tabular orebodies that are vertical or sub-vertical

A

pipes or chimneys

17
Q

Horizontal or subhorizontal tabular orebodies

18
Q

Ore minerals are peppered throughout the body of the host rock in the same way as accessory minerals are disseminated through igneous rock; in fact, they often are accessory minerals.

A

Disseminated orebodies

19
Q

Closed-spaced veinlets cutting the host rock forming an interlacing network

20
Q

Mineralization of this type generally fades _____ into sub-economic mineralization and the boundaries of the orebody are assay limits.

A

gradually outwards

21
Q

(Skarn or contact metamorphic or pyrometasomatic or replacement deposit) Mineralogy

A

calc-silicate minerals
- diopside
- wollastonite
- andradite garnet
- actinolite

22
Q

(Skarn or contact metamorphic or pyrometasomatic or replacement deposit) Ore Mineralogy

A
  • iron
  • copper
  • tungsten
  • graphite
  • zinc
  • lead
  • molybdenum
  • tin
  • uranium
  • talc
23
Q

these orebodies show a considerable development in two dimensions, parallel to the bedding and perpendicular to it, referred to as stratiform.

A

Sedimentary host rocks

24
Q

Any type or types of orebody, concordant or discordant, which are restricted to a particular part of the stratigraphical column

25
Parallel to the bedding and perpendicular to it,
Stratiform
26
Sedimentary host rocks e.g
- Limestone hosted - Argillaceous hosted - Arenaceous hosted - Rudaceous hosted (Placer Deposit)
27
Sedimentary iron and manganese formations and evaporites occur scattered through the stratigraphical column where they form very extensive beds conformable with the stratigraphy.
Chemical sediments
28
Volcanic hosts
Volcanogenic Massive sulfides
29
VMS are generally stratiform bodies, _____ or _____, developed at the interfaces between volcanic units or at sedimentary interfaces.
lenticular, sheet-like
30
Plutonic hosts
Layered Mafic Intrusions (LMI)
30
Plutonic hosts (Magmatic Segregation Deposits)
- Layered Mafic Intrusions (LMI) - Layered Cr-Pt MAfic-Ultramafic Complexes -Cu-Ni-Pt Segregation - Anorthosite - Titanium - Ultramafic volcanic rock associations - Cu - Ni
31
Known also as “Mesothermal Au”, “Slate belt-type Au”, “Archean Au”, “deposits related to solution- remobilization”
Orogenic Gold
32
Restricted to the ultramafic rocks of the various ophiolite belts where climatic conditions and physiographic favor laterization processes.
Laterite
33
high iron content, low nickel, cobalt, magnesia, and silica.
Limonite
34
high nickel, cobalt, and magnesia, but low iron content.
Garnierite/Saprolite
35
is an aluminium ore. It is the world's main source of aluminium. It consists mostly of the minerals gibbsite Al(OH)3, boehmite γ-AlO(OH) and diaspore α-AlO(OH), mixed with the two iron oxides goethite and hematite, the clay mineral kaolinite and small amounts of anatase TiO2.
Bauxite
36
Bauxite source rocks
Nepheline Syenite Clay Clayey limestone Clay shales Crystalline gneisses Basalt Alluvium