Seismic evidence for repeated vertical fluid flow through polygonally faulted strata in the Canterbury Basin, New Zealand-Reference-Cited by-同舟云学术

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Seismic evidence for repeated vertical fluid flow through polygonally faulted strata in the Canterbury Basin, New Zealand

Published:2019-11 Issue: Volume:109 Page:317-329
ISSN:0264-8172
Container-title:Marine and Petroleum Geology
language:en
Short-container-title:Marine and Petroleum Geology

Author:

Hoffmann Jasper J.L.^ORCID,Gorman Andrew R.^ORCID,Crutchley Gareth J.^ORCID

Funder

MBIE

University of Otago

Publisher

Elsevier BV

Subject

Stratigraphy,Economic Geology,Geology,Geophysics,Oceanography

Reference80 articles.

1. Hydrocarbon leakage through focused fluid flow systems in continental margins;Anka;Mar. Geol.,2012

2. Focused fluid flow in passive continental margins;Berndt;Philos. Trans. A Math. Phys. Eng. Sci.,2005

3. Polygonal fault systems on the mid-Norwegian margin: a long-term source for fluid flow;Berndt;Subsurf. Sediment Mobil. Geol. Soc. Lond. Spec. Publ.,2003

4. RV SONNE Fahrtbericht/Cruise Report SO226-CHRIMP CHatham RIse Methane Pockmarks;Bialas,2013

5. Caravel-1: lessons learned in the deepwater Canterbury basin;Blanke,2015

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