Lec 4 - Controls On Ore Deposition Flashcards

1
Q

4 controls on Ore Deposition

A
  1. Chemical
  2. Lithological
  3. Stratgraphic
  4. Structural
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2
Q

Factors under chemical

A
  • temperature change
  • pressure change
  • reaction between solution and wall rocks
  • chemical changes due to solution mixing
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3
Q
  • It affects mineral solubilities,
  • influences ion-pairing hydrolysis constants of ions such as Cl and HS
  • affects oxyfen fugacit
A

Temperature change (cooling)

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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 volatiles without change in temperature but only in pressure

A

Retrograde Boiling

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7
Q
  • Addition of anions or cause of disolution

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

A

Solution mixing

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8
Q

T and P drop will result in precipitation from aqueous solution

A

Solubility

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9
Q

Separation of one mineral from another in a natural solution (unmixing)

A

Exsolution

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10
Q

Certain microbes are agents of mineral precipitation

A

Bacterial precipitation

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11
Q

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

A

Replacement

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12
Q

Loss and gaiin of electrons to specific ions

A

Oxidation and reduction

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13
Q

In openspace without outright replacement

A

Direct Deposition

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14
Q

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

A

Adsorption

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16
Q

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

A

Base exchange

17
Q

Rate of pore volume to the total volume of rock

18
Q

Necessary for passage of solutions through host rock to depositional sites
-main factor of localization in absence of fracture

A

Premeability

19
Q

Brittle rocks crackle readily

A

High permeability

20
Q

Ductile rocks do not crackle

A

Less permeable

21
Q

Thick accumulation of sediments in orogenic environments

A

Geosynclines

22
Q

Regional loci of ore deposition, deposition cluster within or about stocks or batholiths

A

Igneous Intrusions

23
Q

Weathered zones beneath unconformities are more porous, control location of syngenetic sedimentary deposits

A

Unconformities

24
Q

Permeable pathways, replacement or metasomatic deposits extend or deposit along these_____

A

Bedding

*cross bedding are more favorable

25
Serves as barriers for mineralizing solutions; concentrate mineral deposition in strata below or above
Impervious Layer
26
Supergene Sulfides deposits at
Above Impervious layers
27
* The most important loci of ore * Provides zone of porosity and permeability * provides channelways for hydrothermal fluid to pass
Structural
28
Broader localization of ore belts/mineral districts
Regiona
29
Immediate localization of ore
Detailed
30
Cupolas, deposits can be located if fluid is lighter than magma
Structural Highs
31
Cut of a stock dome
Cupolas
32
Lopoliths, sulfide melt is heavier than silicate melt so located at bottomof intrusives
Structural Lows
33
Fold axes with increased fracturing provided channel ways for pre-ore deposition
Folds
34
- Control deposition of ore deposits | - Can result from regional stresses
Fractures / Lineament
35
When your ore deposits in a structural intersection
Ore shoot
36
- favorable for deposition - increased permeability - loci for interaction of different fluids
Structural intersection
37
Faults that occur before deposition if ore minerals, Controlling structure
Syngenetic Faults
38
The deposition of ore minerals happened first before faulting, it cut and displaces ore bodies
Epigenetic Faults
39
High veolocity explosion vent
Diatremes