A petrographic and geochemical model for the origin of calcite cap rock at Damon Mound salt dome, Texas, U.S.A
Calcite cap rock at Damon Mound, Texas, consists of five calcite generations recognizable through standard petrography and cathodoluminescence. Stage-IA calcite formed by dissolution of anhydrite followed by calcite precipitation and was partly replaced by stage-IB calcite. Stage II formed above sta...
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Veröffentlicht in: | Chemical geology 1988-12, Vol.74 (1), p.67-97 |
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Sprache: | eng |
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