Complexity of the 2016 M 7.8 Kaikōura, New Zealand, earthquake from seismic observation: Inferences of overpressured fluid involvement

Author:

Okada Tomomi,Matsuno Miu,Matsumoto Satoshi,Kawamura Yuta,Iio Yoshihisa,Sato Tadashi,Tagami Ayaka,Hirahara Satoshi,Kimura Shuutoku,Bannister Stephen,Ristau John,Savage Martha K.,Thurber Clifford H.,Sibson Richard H.

Funder

Japan Society for the Promotion of Science

Government of Japan Ministry of Education Culture Sports Science and Technology

National Science Foundation

Earthquake Commission

Publisher

Elsevier BV

Reference63 articles.

1. Characterization of barriers on an earthquake fault;Aki;J. Geophys. Res.,1979

2. Dynamic rupture simulation reproduces spontaneous multifault rupture and arrest during the 2016 M w 7.9 Kaikōura earthquake;Ando;Geophys. Res. Lett.,2018

3. Two regions of seafloor deformation generated the tsunami for the 13 November 2016, Kaikōura, New Zealand earthquake;Bai;Geophys. Res. Lett.,2017

4. Stress and crustal anisotropy in Marlborough, New Zealand: evidence for low fault strength and structure-controlled anisotropy;Balfour;Geophys. J. Int.,2005

5. Complex rupture process of the mw 7.8, 2016, Kaikōura earthquake, New Zealand, and its aftershock sequence;Cesca;Earth Planet. Sci. Lett.,2017

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