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Title: Oil field brines as ore-forming solutions

Journal Article · · Econ. Geol.; (United States)

The hypothesis that oil field brines can become ore-forming solutions and can transport base metals and reduced sulfur to sites of ore formation by large-scale migration along aquifers out of sedimentary basins is examined using data on the chemical compositions of presnt-day heavy metal-bearing oil field brines and the petrography of their reservoir rocks, and is a theoretical evaluation of the chemistry of possible water-rock interactions in the aquifers during migration. The concept of water-rock interactions in the aquifers of sandstone and carbonate-hosted base metal sulfide ore deposits is clearly of potential importance in explaining geochemical characteristics of such deposits, including the Na/K ratios of the fluid inclusions, the lead isotope compositions of galena, the paragenesis sphalerite followed by galena, and the overall Zn/Pb ratios of the deposits. It is because of these water-rock interactions that a single brine carrying base metals and reduced sulfur can evolve chemically in its aquifer so that brines with a spectrum of geochemical characteristics arrive as a function of time at a distant site of ore formation.

Research Organization:
Dept. of Earth and Space Sciences, State Univ. of New York at Stony Brook, Stony Brook, NY
OSTI ID:
6641700
Journal Information:
Econ. Geol.; (United States), Vol. 79:1
Country of Publication:
United States
Language:
English