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Volumn 16, Issue 7, 1988, Pages 641-644
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Chemical model for the origin of minor limestone-shale cycles by anaerobic methane oxidation
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Author keywords
[No Author keywords available]
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Indexed keywords
ISOTOPES;
LIME;
LIMESTONE;
METHANE;
OXIDATION;
PYRITES;
SULFUR COMPOUNDS;
ANAEROBIC METHANE OXIDATIONS;
CARBONATE CONCRETION;
CHEMICAL MODEL;
DEPTH VARIATION;
ISOTOPIC CHARACTERISTICS;
ISOTOPIC STUDY;
SEDIMENTATION RATES;
SULFATE REDUCTION;
SHALE;
CARBONATE;
CHEMICAL COMPOSITION;
CONCRETION;
JURASSIC;
METHANE;
OXIDATION;
PYRITE;
SEDIMENTATION RATE;
SULFATE;
SUPERSATURATION;
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EID: 0001690833
PISSN: 00917613
EISSN: 19432682
Source Type: Journal
DOI: 10.1130/0091-7613(1988)016<0641:CMFTOO>2.3.CO;2 Document Type: Article |
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Times cited : (135)
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References (0)
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