Two regions of seafloor deformation generated the tsunami for the 13 November 2016, Kaikoura, New Zealand earthquake-Reference-Cited by-同舟云学术

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Two regions of seafloor deformation generated the tsunami for the 13 November 2016, Kaikoura, New Zealand earthquake

Published:2017-07-03 Issue:13 Volume:44 Page:6597-6606
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Bai Yefei¹^ORCID,Lay Thorne²^ORCID,Cheung Kwok Fai¹^ORCID,Ye Lingling³^ORCID

Affiliation:

1. Department of Ocean and Resources Engineering University of Hawaii at Manoa Honolulu Hawaii USA

2. Department of Earth and Planetary Sciences University of California Santa Cruz Santa Cruz California USA

3. Seismological Laboratory, California Institute of Technology Pasadena California USA

Funder

National Oceanic and Atmospheric Administration

National Sleep Foundation

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/2017GL073717

Reference37 articles.

1. Tsunami surges around the Hawaiian Islands from the 1 April 2014 North Chile M w 8.1 earthquake

2. Interconnection of multi-scale standing waves across the Pacific Basin from the 2011 Tohoku Tsunami

3. Hikurangi margin tsunami earthquake generated by slow seismic rupture over a subducted seamount

4. Ground‐Motion Observations from the 14 November 2016Mw 7.8 Kaikoura, New Zealand, Earthquake and Insights from Broadband Simulations

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