Simple Physical Model for the Probability of a Subduction- Zone Earthquake Following Slow Slip Events and Earthquakes: Application to the Hikurangi Megathrust, New Zealand-Reference-Cited by-同舟云学术

Simple Physical Model for the Probability of a Subduction- Zone Earthquake Following Slow Slip Events and Earthquakes: Application to the Hikurangi Megathrust, New Zealand

Published:2018-05-08 Issue:9 Volume:45 Page:3932-3941
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Kaneko Yoshihiro¹^ORCID,Wallace Laura M.¹²^ORCID,Hamling Ian J.¹^ORCID,Gerstenberger Matthew C.¹

Affiliation:

1. GNS Science; Lower Hutt New Zealand

2. Institute for Geophysics; University of Texas at Austin; Austin TX USA

Funder

Government of New Zealand

Royal Society of New Zealand's Rutherford Discovery Fellowship

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1029/2018GL077641/fullpdf

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3. Re-estimated effects of deep episodic slip on the occurrence and probability of great earthquakes in Cascadia;Beeler;Bulletin of the Seismological Society of America,2013

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5. Evidence for past subduction earthquakes at a plate boundary with widespread upper plate faulting: Southern Hikurangi margin, New Zealand;Clark;Bulletin of the Seismological Society of America,2015

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