Regional uplift, gas hydrate dissociation and the origins of the Paleocene-Eocene Thermal Maximum

Earth and Planetary Science Letters

Volumn 245, Issue 1-2, 2006, Pages 65-80

  Maclennan, John ^a   Jones, Stephen M ^b  

^a UNIVERSITY OF CAMBRIDGE   (United Kingdom)

^b TRINITY COLLEGE DUBLIN   (Ireland)

Author keywords

gas hydrates; North Atlantic Igneous Province; Paleocene Eocene Thermal Maximum; rapid climate change; regional uplift

Indexed keywords

CARBON ISOTOPE; GAS HYDRATE DISSOCIATION; PALEOCENE-EOCENE THERMAL MAXIMUM; RAPID CLIMATE CHANGE; REGIONAL UPLIFT;

CARBON; CLIMATE CHANGE; GAS HYDRATES; GEOCHRONOLOGY; GREENHOUSE EFFECT; ISOTOPES; MATHEMATICAL MODELS; STRATIGRAPHY;

STRUCTURAL GEOLOGY;

CLIMATE CHANGE; GAS HYDRATE; HYPSITHERMAL; PALEOCENE-EOCENE BOUNDARY; UPLIFT;

EID: 33646178084     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.epsl.2006.01.069     Document Type: Article

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