Controls on Ore Deposition Flashcards

1
Q

Controls on Ore Deposition

A

Chemical

Lithologic

Stratigraphic

Structural

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2
Q

Chemical Controls

A

temp change

pressure change

reaction between solution and wallrocks

chem changes due to solution mixing

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3
Q

Temperature Change (Cooling)

will

A

affect mineral solubilities

affect stabilities of aqueous metal bearing complex ions

influence io-pairing hydrolysis constants of ions

affect oxygen fugacity

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4
Q

loss of volatiles disabling metal transport

A

Boiling

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5
Q

change in pressure regime from lithostatic to hydrostatic across an obstruction

A

Throttling

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6
Q

loss of H+ and H2O, increase Na+ and Ca+2

A

hydrolysis and hydration

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7
Q

loss of volatiles disabling metal transport without change in temperature

A

Retrograde

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8
Q

can cause precipitation by causing dissociation of some metal complexes and recombination

A

Dilution

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9
Q

T & P drop will result in precipitation from aqueous solution

A

Solubility

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10
Q

separation of one mineral from another in a natural solution

A

Exsolution

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11
Q

certain microbes are agents of mineral precipitation

A

Bacterial Precipitation

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12
Q

simultaneous capillary solution and deposition by which new minerals are substituted for earlier minerals or rocks

A

Replacement

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13
Q

loss and gain of electrons to specific ions

A

Oxidation and Reduction (redox)

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14
Q

certain substances cause precipitation from solution without themselves entering into solution

A

Catalytic Action

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15
Q

taking up of one substance at the surface of another

kaolin absorbing copper to form chrysocolla

A

Adsorption

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16
Q

occurs between solids and liquids whereby cations are exchanged, producing changed characteristics of both

A

Base Exhchange

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17
Q

ratio of pore volume to the total volume of rock

18
Q

necessary for passage of solution through host rock to depositional sites

A

Permeability

19
Q

High Permeable Rocks

A

Rhyolite/Quartzite/Limestone/Silicified Rocks

20
Q

Less Permeable Rocks

A

Shale/Schist/Basaltic Rocks/ Chloritized Rocks

21
Q

some constituents in rocks are more reactive

A

Composition

22
Q

thick accumulation of sediments in orogenic environments

A

Geosynclines

23
Q

regional loci of ore deposition

-deposits cluster within or about stocks or batholiths

A

Igneous Intrusions

24
Q

it is related to uplift, folding, faulting, and intrusion

A

geosynclines

25
control location of syngenetic sedimentary deposits
Unconformitites
26
are permeable pathways replacement or metasomatic deposits extend or deposit along it
Bedding
27
serve as barriers for mineralizing solutions: Concentrate deposition in strata below or above
Impervious Layers (Covers and bases)
28
most important loci of ore
Structural Control
29
broader localization of ore belts/mineral districts
Regional
30
immediate localization of ore
Detailed
31
provide zones of porosity and permeability
structural control
32
deposits can be located if fluid is lighter than magma
Structural highs - cupolas (cut of a stock dome)
33
sulfide melt is heavier than silicate melt so located at bottom of intrusive
Structural Lows -lopoliths
34
axes with increased fracturing provide channelways for pre-ore depostion
Folds
35
control deposition of ore deposits can result from regional stresses
Fractures/Lineaments
36
favorable for deposition increased permeability loci for interaction of different fluids
Structural Intersections
37
controlling structure
Syngenetic
38
a high velocity volcanic explosion vent
diatreme
39
physical and chemical properties of host rocks exact properties are seldom evident operate along with structural features
lithologic control
40
cut and displace ore bodies change attitude, width, and grades of ores
Epigenetic