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Volumn 10, Issue 6, 1995, Pages 965-971
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Dissociation of oceanic methane hydrate as a cause of the carbon isotope excursion at the end of the Paleocene
a a a a
a
NONE
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Author keywords
[No Author keywords available]
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Indexed keywords
CARBON;
ISOTOPE;
METHANE;
WATER;
CARBON ISOTOPE;
GAS HYDRATE;
ISOTOPIC EXCURSION;
METHANE;
PALAEOCEANOGRAPHY;
PALAEOCENE;
THERMAL MAXIMUM;
ATMOSPHERE;
DISSOCIATION;
GAS;
HYPOTHESIS;
PALEOCEANOGRAPHY;
PALEOCENE;
SEA;
SEDIMENT;
WARMING;
WATER TEMPERATURE;
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EID: 0029529085
PISSN: 08838305
EISSN: 19449186
Source Type: Journal
DOI: 10.1029/95PA02087 Document Type: Article |
Times cited : (1155)
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References (44)
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