Clay assemblage and oxygen isotopic constraints on the weathering response to the Paleocene-Eocene thermal maximum, east coast of North America
Author:
Publisher
Geological Society of America
Subject
Geology
Reference20 articles.
1. Palaeocene- early Eocene climatic evolution in the Tethyan realm: clay mineral evidence
2. A humid climate state during the Palaeocene/Eocene thermal maximum
3. Terrestrial records of a regional weathering profile at the Paleocene-Eocene boundary in the Williston Basin of North Dakota
4. Dissociation of oceanic methane hydrate as a cause of the carbon isotope excursion at the end of the Paleocene
5. Stratigraphic and climatic implications of clay mineral changes around the Paleocene/Eocene boundary of the northeastern US margin
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