DISSOCIATION OF OCEANIC METHANE HYDRATE AS A CAUSE OF THE CARBON-ISOTOPE EXCURSION AT THE END OF THE PALEOCENE
DISSOCIATION OF OCEANIC METHANE HYDRATE AS A CAUSE OF THE CARBON-ISOTOPE EXCURSION AT THE END OF THE PALEOCENE
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DOI：
10.1029/95pa02087
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发表时间：
1995-12-01
期刊：
影响因子：
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通讯作者：
OWEN, RM
中科院分区：
文献类型：
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作者：
DICKENS, GR;ONEIL, JR;OWEN, RM
“最新古新世热极大值”（LPTM）的同位素记录表明，在短暂的时间间隔内，底层水温上升了4摄氏度以上（
Isotopic records across the ''Latest Paleocene Thermal Maximum'' (LPTM) indicate that bottom water temperature increased by more than 4 degrees C during a brief time interval (