Lec 4 - Controls On Ore Deposition Flashcards
4 controls on Ore Deposition
- Chemical
- Lithological
- Stratgraphic
- Structural
Factors under chemical
- temperature change
- pressure change
- reaction between solution and wall rocks
- chemical changes due to solution mixing
- It affects mineral solubilities,
- influences ion-pairing hydrolysis constants of ions such as Cl and HS
- affects oxyfen fugacit
Temperature change (cooling)
Loss of volatiles disabling metal transport
Boiling
Change in pressure regime from lithostatic to hydrostatic across an obstruction
Throttling
Loss of volatiles without change in temperature but only in pressure
Retrograde Boiling
- Addition of anions or cause of disolution
- disolution can cause precipitation by causing dissociation of some metal complexes and recombination
Solution mixing
T and P drop will result in precipitation from aqueous solution
Solubility
Separation of one mineral from another in a natural solution (unmixing)
Exsolution
Certain microbes are agents of mineral precipitation
Bacterial precipitation
Simultaneous capillary solution and deposition by which new minerals are substituted for earlier mineral or rocks
Replacement
Loss and gaiin of electrons to specific ions
Oxidation and reduction
In openspace without outright replacement
Direct Deposition
Precipitation from solution without themselves entering into solution
Catalytic action
Taking up of one substance at the surface of another
Adsorption