High-resolution resistivity imaging of marine gas hydrate structures by combined inversion of CSEM towed and ocean-bottom receiver data

Author:

Attias Eric1ORCID,Weitemeyer Karen1,Hölz Sebastian2,Naif Samer3,Minshull Tim A1,Best Angus I4,Haroon Amir2,Jegen-Kulcsar Marion2,Berndt Christian2

Affiliation:

1. Ocean and Earth Science, National Oceanography Centre Southampton, University of Southampton, Southampton SO14 3ZH, UK

2. GEOMAR Helmholtz Centre for Ocean Research, Marine Geodynamics, 24148 Kiel, Germany

3. Lamont Doherty Earth Observatory, Columbia University, Palisades, NY 10964, USA

4. National Oceanography Centre, University of Southampton Waterfront Campus, Southampton SO14 3ZH, UK

Publisher

Oxford University Press (OUP)

Subject

Geochemistry and Petrology,Geophysics

Reference98 articles.

1. Methane hydrate stability and anthropogenic climate change;Archer;Biogeosciences Discuss.,2007

2. Ocean methane hydrates as a slow tipping point in the global carbon cycle;Archer;Proc. Natl. Acad. Sci. USA,2009

3. CSEM towed receiver data from Nyegga, CNE03 pockmark;Attias;PANGAEA: Data Publiser for Earth & Environmental Science,2017

4. Controlled-source electromagnetic and seismic delineation of subseafloor fluid flow structures in a gas hydrate province, offshore Norway;Attias;Geophys. J. Int.,2016

5. Current perspectives on gas hydrate resources;Boswell;Energy Environmental Sci.,2011

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