Evolution of metal ratios and δ34S composition of sulfide mineralization during anhydrite cap rock formation, Hockley Dome, Texas, U.S.A.-Reference-Cited by-同舟云学术

Evolution of metal ratios and δ34S composition of sulfide mineralization during anhydrite cap rock formation, Hockley Dome, Texas, U.S.A.

Published:1988-12 Issue:1-2 Volume:74 Page:37-55
ISSN:0009-2541
Container-title:Chemical Geology
language:en
Short-container-title:Chemical Geology

Author:

Kyle J.Richard,Agee William N.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference37 articles.

1. Gulf Coast formation waters as potential source fluids for cap rock-hosted sulfide mineralization Hockley Dome, Texas;Agee;Gulf Coast Assoc. Geol. Soc. Trans.,1988

2. Solubilities of ore minerals;Barnes,1979

3. Geologic Atlas of Texas, Houston Sheet;Barnes,1968

4. Fault leaked H2S and the origin of south Texas uranium deposits: implications of sulfur isotopic studies;Busche,1982

5. Preliminary report on the origin and chemical evolution of lead- and zinc-rich oil field brines in central Mississippi;Carpenter;Econ. Geol.,1974

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