Chemical controls on solubility of ore-forming minerals in hydrothermal solutions.

D. Crerar, S. Wood, S. Brantley, A. Bocarsly

Research output: Contribution to journalArticle

108 Citations (Scopus)

Abstract

The transport, deposition and zoning of hydrothermal ores are controlled by the crystal chemistry and stability of their minerals, the physicochemical properties of aqueous electrolyte solutions at high T and P, and the thermodynamic and molecular properties of aqueous species of metals. Recent solubility and spectroscopic data indicate that for transition-metal complexes at elevated T, bonding changes from primarily ionic to covalent from left to right across each transition row. The Pearson rule successfully describes speciation to about 250oC, but breaks down at high T as all metals become harder, and electrostatic interaction increases. Relativistic effects predict an increased tendency toward covalent bonding down each vertical group of elements; this in part explains the preference of Au and Hg for HS- complexes and may also explain the apparent differences in speciation between Sb and Bi. Ligation numbers decrease with T, and neutral complexes like 038FeCl20 predominate above approx 300oC due to decreasing dia-electric constant of water, change from octahedral to tetrahedral complex coordination, pronounced decrease in activity of anionic ligands, and increasing importance of hydrolysis. Increased solubility of ore minerals at higher-T can be attributed to some of the above effects and, also, to the temperature dependence of oxygen and sulphur fugacities and of pH buffer capacity. The buffer capacity also depends on solute composition and may help explain the rapid precipitation of minerals in porphyry-type ores and the more gradual precipitation in Mississippi-Valley-type deposits.-L.C.C.

Original languageEnglish (US)
Pages (from-to)333-352
Number of pages20
JournalCanadian Mineralogist
Volume23
Issue number3
StatePublished - Jan 1 1985

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chemical control
Ores
Minerals
solubility
Solubility
Coordination Complexes
Mississippi Valley-type deposit
crystal chemistry
metal
ore mineral
Buffers
transition element
physicochemical property
mineral
fugacity
porphyry
electrolyte
ligand
Crystal chemistry
zoning

All Science Journal Classification (ASJC) codes

  • Geochemistry and Petrology

Cite this

Crerar, D. ; Wood, S. ; Brantley, S. ; Bocarsly, A. / Chemical controls on solubility of ore-forming minerals in hydrothermal solutions. In: Canadian Mineralogist. 1985 ; Vol. 23, No. 3. pp. 333-352.
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Chemical controls on solubility of ore-forming minerals in hydrothermal solutions. / Crerar, D.; Wood, S.; Brantley, S.; Bocarsly, A.

In: Canadian Mineralogist, Vol. 23, No. 3, 01.01.1985, p. 333-352.

Research output: Contribution to journalArticle

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