Dissociation of oceanic methane hydrate as a cause of the carbon isotope excursion at the end of the Paleocene
Year: 1995
Type: article
Source: Paleoceanography
DOI: 10.1029/95pa02087
Language: English
Subfield: Environmental Chemistry
Field: Environmental Science
Domain: Physical Sciences
SDG: Climate action
Open Access status: closed
OpenAlex ID: W2094953080
