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Volumn 89, Issue 4, 1994, Pages 858-876
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Origin of dissolution vugs, caverns, and breccias in the Middle Devonian Presqu'ile barrier, host of Pine Point Mississippi Valley- type deposits
a a |
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Author keywords
[No Author keywords available]
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Indexed keywords
DISSOLUTION;
HYDROTHERMAL FLUID;
LEAD;
METEORIC FLUID;
MINERALIZATION;
MISSISSIPPI VALLEY TYPE DEPOSIT;
ZINC;
CANADA;
NORTHWEST TERRITORIES;
PINE POINT;
BRECCIAS;
CAVERNS;
DIAGENESIS;
DOLOMITES;
DOLOMITIZATION;
FLUID INCLUSION MEASUREMENTS;
METEORIC KARSTIFICATION;
THERMOCHEMICAL SULFATE REDUCTION;
VUGS;
BRINES;
CARBONATE MINERALS;
CEMENTS;
DISSOLUTION;
GEOGRAPHICAL REGIONS;
LIMESTONE;
ORE DEPOSIT GEOLOGY;
PRECIPITATION (CHEMICAL);
REDUCTION;
ROCKS;
SHALE;
SODIUM CHLORIDE;
LEAD ZINC DEPOSITS;
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EID: 0028443712
PISSN: 03610128
EISSN: None
Source Type: Journal
DOI: 10.2113/gsecongeo.89.4.858 Document Type: Article |
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Times cited : (51)
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References (0)
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