Mineral Deposit Geology and Models Flashcards

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

A

mantos

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

A

stockwork

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

A

Strata-bound

25
Q

Parallel to the bedding and perpendicular to it,

A

Stratiform

26
Q

Sedimentary host rocks e.g

A
  • Limestone hosted
  • Argillaceous hosted
  • Arenaceous hosted
  • Rudaceous hosted (Placer Deposit)
27
Q

Sedimentary iron and manganese formations and evaporites occur scattered through the stratigraphical column where they form very extensive beds conformable with the stratigraphy.

A

Chemical sediments

28
Q

Volcanic hosts

A

Volcanogenic Massive sulfides

29
Q

VMS are generally stratiform bodies, _____ or _____, developed at the interfaces between volcanic units or at sedimentary interfaces.

A

lenticular, sheet-like

30
Q

Plutonic hosts

A

Layered Mafic Intrusions (LMI)

30
Q

Plutonic hosts (Magmatic Segregation Deposits)

A
  • Layered Mafic Intrusions (LMI)
  • Layered Cr-Pt MAfic-Ultramafic Complexes
    -Cu-Ni-Pt Segregation
  • Anorthosite - Titanium
  • Ultramafic volcanic rock associations - Cu - Ni
31
Q

Known also as “Mesothermal Au”, “Slate belt-type Au”, “Archean Au”, “deposits related to solution-
remobilization”

A

Orogenic Gold

32
Q

Restricted to the ultramafic rocks of the various ophiolite belts where climatic conditions and physiographic favor laterization processes.

A

Laterite

33
Q

high iron content, low nickel, cobalt, magnesia, and silica.

A

Limonite

34
Q

high nickel, cobalt, and magnesia, but low iron content.

A

Garnierite/Saprolite

35
Q

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.

A

Bauxite

36
Q

Bauxite source rocks

A

Nepheline Syenite
Clay
Clayey limestone
Clay shales
Crystalline gneisses
Basalt
Alluvium