1. Ore deposit environments
Magmatic
Cumulate deposits – fractional crystallization processes can concentrate metals (Cr, Fe, Pt)
Pegmatites – late staged crystallization forms pegmatites and many residual elements are concentrated (Li, Ce, Be, Sn, and U)
Hydrothermal
Magmatic fluid - directly associated with magma
Porphyries - Hot water heated by pluton
Skarn – hot water associated with contact metamorphisms
Exhalatives – hot water flowing to surface
Epigenetic – hot water not directly associated with pluton

2. Water-rock interactions
To concentrate a material, water must:
Transport the ions
A ‘trap’ must cause precipitation in a spatially constrained manner
Trace metals which do not go into igneous minerals easily get very concentrated in the last bit of melt
Leaching can preferentially remove materials, enriching what is left or having the leachate precipitate something further away

3. Metal Sulfide Mineral Solubility
Problem 1: Transport of Zn to ‘trap’:
ZnS + 2 H O2 = Zn2+ + S2- + H2O
Need to determine the redox state the Zn2+ would have been at equilibrium with…
What other minerals are in the deposit that might indicate that?  define approximate fO2 and fS2- values and compute Zn2+ conc.  Pretty low Zn2+

4. Must be careful to consider what the conditions of water transporting the metals might have been  how can we figure that out??
What other things might be important in increasing the amount of metal a fluid could carry? More metal a fluid can hold the quicker a larger deposit can be formed…

5. How about the following:
ZnS + 2 H O2 + Cl- = ZnCl+ + S2- + H2O
Compared to
That is a BIG difference…

6. Geochemical Traps
Similar to chemical sedimentary rocks – must leach material into fluid, transport and deposit ions as minerals…
pH, redox, T changes and mixing of different fluids results in ore mineralization
Cause metals to go from soluble to insoluble
Sulfide (reduced form of S) strongly binds metals  many important metal ore minerals are sulfides!

7. Piquette Mine
1-5 nm particles of FeOOH and ZnS – biogenic precipitation
Tami collecting samples

8. cells
ZnS

9. Piquette Mine – SRB activity
At low T, thermochemical SO42- reduction is WAY TOO SLOW – microbes are needed!
‘Pure’ ZnS observed, buffering HS- concentration by ZnS precipitation

10. Fluid Flow and Mineral Precipitation
monomineralic if:
flux Zn2+ > HS- generation
i.e.  there is always enough Zn2+ transported to where the HS- is generated, if
sequential precipitation if:
Zn2+ runs out then HS- builds until PbS precipitates
ZnS
ZnS
x Zn2+
y Pb2+
Monomineralic precipitation of ZnS may occur if flux of metal in this system does not outstrip HS- generation, other sulfides (PbS then FeS) will form if the Zn2+ is removed from the system and HS- builds to a point where the mext metal sulfide foms
ZnS
PbS
z HS- generated
by SRB in time t

11. Model Application
Use these techniques to better understand ore deposit formation and metal remediation schemes
This model can then be applied to thinking about the deposition of ore deposits where microbial HS- generation, fluid flow rates, and microbial activity determines the spatial separation of metal sulfide minerals. Minerals may coprecipitate where more than one metal is supersaturated.

12. Sequential Precipitation Experiments
SRB cultured in a 125 ml septum flask containing equimolar Zn2+ and Fe2+
Flask first develops a white precipitate (ZnS) and only develops FeS precipitates after most of the Zn2+ is consumed
Upcoming work in my lab will investigate this process using microelectrodes  where observation of ZnS and FeS molecular clusters will be possible!

13. Hydrothermal Ore Deposits
Thermal gradients induce convection of water – leaching, redox rxns, and cooling create economic mineralization

14. Ore deposit environments
Sedimentary
Placer – weathering of primary mineralization and transport by streams (Gold, diamonds, other)
Banded Iron Formations – 90%+ of world’s iron tied up in these (more later…)
Evaporite deposits – minerals like gypsum, halite deposited this way
Laterites – leaching of rock leaves residual materials behind (Al, Ni, Fe)
Supergene – reworking of primary ore deposits remobilizes metals (often over short distances)