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      Shallow methane hydrate system controls ongoing, downslope sediment transport in a low-velocity active submarine landslide complex, Hikurangi Margin, New Zealand

      , , , , ,
      Geochemistry, Geophysics, Geosystems
      Wiley-Blackwell

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          Gas hydrates-geological perspective and global change

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            Subduction zone coupling and tectonic block rotations in the North Island, New Zealand

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              • Record: found
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              Escape of methane gas from the seabed along the West Spitsbergen continental margin

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                Author and article information

                Journal
                Geochemistry, Geophysics, Geosystems
                Geochem. Geophys. Geosyst.
                Wiley-Blackwell
                15252027
                November 2014
                November 07 2014
                : 15
                : 11
                : 4137-4156
                Article
                10.1002/2014GC005379
                8acdf4c5-27b5-49d9-8aa1-93012fbd31d0
                © 2014

                http://doi.wiley.com/10.1002/tdm_license_1.1

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