Upward‐Doming Zones of Gas Hydrate and Free Gas at the Bases of Gas Chimneys, New Zealand's Hikurangi Margin-Reference-Cited by-同舟云学术

Upward‐Doming Zones of Gas Hydrate and Free Gas at the Bases of Gas Chimneys, New Zealand's Hikurangi Margin

Published:2021-09 Issue:9 Volume:126 Page:
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J Geophys Res Solid Earth

Author:

Crutchley G. J.¹^ORCID,Mountjoy J. J.²^ORCID,Hillman J. I. T.³^ORCID,Turco F.⁴^ORCID,Watson S.²^ORCID,Flemings P. B.⁵^ORCID,Davy B.³^ORCID,Woelz S.²^ORCID,Gorman A. R.⁴^ORCID,Bialas J.¹^ORCID

Affiliation:

1. GEOMAR Helmholtz Centre for Ocean Research Kiel Kiel Germany

2. National Institute of Water and Atmospheric Research Wellington New Zealand

3. GNS Science Lower Hutt New Zealand

4. University of Otago Dunedin New Zealand

5. Jackson School of Geosciences University of Texas at Austin Austin TX USA

Funder

Ministry for Business Innovation and Employment

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020JB021489

Reference72 articles.

1. Gas Hydrates ‐ Part V: The Resource Potential;Amundsen L.;GEOExPro magazine,2015

2. Evolution of the Upper Cenozoic Magmatic Arc and plate boundary in northern New Zealand

3. Strain partitioning in the transition area between oblique subduction and continental collision;Barnes P. M.;Hikurangi margin, New Zealand: Tectonics,1998

4. Tectonic and geological framework for gas hydrates and cold seeps on the Hikurangi subduction margin, New Zealand

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