Controls on Ore Deposition Flashcards
Controls on Ore Deposition
Chemical
Lithologic
Stratigraphic
Structural
Chemical Controls
temp change
pressure change
reaction between solution and wallrocks
chem changes due to solution mixing
Temperature Change (Cooling)
will
affect mineral solubilities
affect stabilities of aqueous metal bearing complex ions
influence io-pairing hydrolysis constants of ions
affect oxygen fugacity
loss of volatiles disabling metal transport
Boiling
change in pressure regime from lithostatic to hydrostatic across an obstruction
Throttling
loss of H+ and H2O, increase Na+ and Ca+2
hydrolysis and hydration
loss of volatiles disabling metal transport without change in temperature
Retrograde
can cause precipitation by causing dissociation of some metal complexes and recombination
Dilution
T & P drop will result in precipitation from aqueous solution
Solubility
separation of one mineral from another in a natural solution
Exsolution
certain microbes are agents of mineral precipitation
Bacterial Precipitation
simultaneous capillary solution and deposition by which new minerals are substituted for earlier minerals or rocks
Replacement
loss and gain of electrons to specific ions
Oxidation and Reduction (redox)
certain substances cause precipitation from solution without themselves entering into solution
Catalytic Action
taking up of one substance at the surface of another
kaolin absorbing copper to form chrysocolla
Adsorption
occurs between solids and liquids whereby cations are exchanged, producing changed characteristics of both
Base Exhchange
ratio of pore volume to the total volume of rock
Porosity
necessary for passage of solution through host rock to depositional sites
Permeability
High Permeable Rocks
Rhyolite/Quartzite/Limestone/Silicified Rocks
Less Permeable Rocks
Shale/Schist/Basaltic Rocks/ Chloritized Rocks
some constituents in rocks are more reactive
Composition
thick accumulation of sediments in orogenic environments
Geosynclines
regional loci of ore deposition
-deposits cluster within or about stocks or batholiths
Igneous Intrusions
it is related to uplift, folding, faulting, and intrusion
geosynclines