Time-dependent modeling of slow slip events and associated seismicity and tremor at the Hikurangi subduction zone, New Zealand-Reference-Cited by-同舟云学术

Time-dependent modeling of slow slip events and associated seismicity and tremor at the Hikurangi subduction zone, New Zealand

Published:2014-01 Issue:1 Volume:119 Page:734-753
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res. Solid Earth

Author:

Bartlow Noel M.¹²,Wallace Laura M.³,Beavan R. John⁴⁵,Bannister Stephen⁴,Segall P.¹

Affiliation:

1. Department of Geophysics; Stanford University; Stanford California USA

2. Now at Institute of Geophysics and Planetary Physics, Scripps Institution of Oceanography; University of California San Diego; La Jolla California USA

3. Institute for Geophysics; University of Texas at Austin; Austin Texas USA

4. GNS Science; Lower Hutt New Zealand

5. Deceased 19 November 2012

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference67 articles.

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3. Seismic evidence for overpressured subducted oceanic crust and megathrust fault sealing;Audet;Nature,2009

4. Variability in earthquake stress drop and apparent stress;Baltay;Geophys. Res. Lett.,2011

5. Geometry of the Hikurangi subduction thrust and upper plate, North Island, New Zealand;Barker;Geochem. Geophys. Geosyst.,2009

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