Anatomy of the 2009 Fiordland earthquake (Mw 7.8), South Island, New Zealand

Mahesh, P. ; Kundu, Bhaskar ; Catherine, J. K. ; Gahalaut, V. K. (2011) Anatomy of the 2009 Fiordland earthquake (Mw 7.8), South Island, New Zealand Geoscience Frontiers, 2 (1). pp. 17-22. ISSN 1674-9871

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Official URL: https://www.sciencedirect.com/science/article/pii/...

Related URL: http://dx.doi.org/10.1016/j.gsf.2010.12.002

Abstract

We have analyzed the July 15, 2009, Fiordland earthquake (Mw 7.8), which occurred in the southwestern part of the South Island of New Zealand. This thrust-related earthquake in the southern Fiordland subduction zone is the largest New Zealand earthquake in the past 80 years. We have constrained a rupture model for this earthquake using coseismic offsets derived from the continuous geodetic network (Global Positioning System) of the New Zealand Institute of Geological and Nuclear Sciences (GNS Science). Our analysis concludes that this earthquake significantly increased the Coulomb stress on the overriding plate, particularly on the offshore portion of the Alpine fault.

Item Type:Article
Source:Copyright of this article belongs to Elsevier Science.
Keywords:Fiordland Subduction Zone; Global Positioning System; Coulomb Stress; Alpine Fault
ID Code:113244
Deposited On:07 Jun 2018 09:12
Last Modified:07 Jun 2018 09:12

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