Shallow-water carbonate responses to the Paleocene-Eocene thermal maximum in the Tethyan Himalaya (southern Tibet): Tectonic and climatic implications
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文摘
The PETM record in shallow marine environment of eastern Tethys ocean The magnitude of negative CIE is ~ 3.4-6‰ for bulk rock and ~ 3‰ for organic matter The origin of P/E disconformity: tectonic or climatic control

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