CO2-driven ocean circulation changes as an amplifier of Paleocene-Eocene thermal maximum hydrate destabilization (2010)

First Author: Lunt D

Abstract

No abstract provided

Bibliographic Information

Digital Object Identifier: http://dx.doi.org/10.1130/G31184.1

Publication URI: http://dx.doi.org/10.1130/G31184.1

Type: Journal Article/Review

Parent Publication: Geology

Issue: 10