Geological controls on focused fluid flow through the gas hydrate stability zone on the southern Hikurangi Margin of New Zealand, evidenced from multi-channel seismic data

Highly concentrated gas hydrate deposits are likely to be associated with geological features that promote increased fluid flux through the gas hydrate stability zone (GHSZ). We conduct conventional seismic processing techniques and full-waveform inversion methods on a multi-channel seismic line tha...

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Veröffentlicht in:	Marine and petroleum geology 2011-11, Vol.28 (10), p.1915-1931
Hauptverfasser:	Crutchley, G.J., Gorman, A.R., Pecher, I.A., Toulmin, S., Henrys, S.A.
Format:	Artikel
Sprache:	eng
Schlagworte:	Anticline Blanking zone Fluid dynamics Fluid flow Fluids Gas hydrate Gas hydrates Geology Hikurangi Margin Inversions Marine Ridges Seismic phenomena Waveform inversion
Online-Zugang:	Volltext
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