Preliminary Analysis of Strong Ground Motions in the Heavily Damaged Zone in Mashiki Town, Kumamoto, Japan, during the Mainshock of the 2016 Kumamoto Earthquake (Mw 7.0) Observed by a Dense Seismic Array

Yoshiya Hata; Hiroyuki Goto; Masayuki Yoshimi

doi:10.1785/0220160107

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Research Article| August 10, 2016

Preliminary Analysis of Strong Ground Motions in the Heavily Damaged Zone in Mashiki Town, Kumamoto, Japan, during the Mainshock of the 2016 Kumamoto Earthquake (⁠ $M_{w}$ 7.0) Observed by a Dense Seismic Array

Yoshiya Hata;

Yoshiya Hata

^a

Graduate School of Engineering, Osaka University, 2‐1, Yamada‐oka, Suita 565‐0871, Japan, [email protected]

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Hiroyuki Goto;

Hiroyuki Goto

^b

Disaster Prevention Research Institute, Kyoto University, Gokasho, Uji, Kyoto 611‐0011, Japan, [email protected]

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Masayuki Yoshimi

^c

Geological Survey of Japan, National Institute of Advanced Industrial Science and Technology, 1‐1‐1 Higashi, Tsukuba 305‐8567, Japan, [email protected]

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Author and Article Information

Yoshiya Hata

^a

Graduate School of Engineering, Osaka University, 2‐1, Yamada‐oka, Suita 565‐0871, Japan, [email protected]

Hiroyuki Goto

^b

Disaster Prevention Research Institute, Kyoto University, Gokasho, Uji, Kyoto 611‐0011, Japan, [email protected]

Masayuki Yoshimi

^c

Geological Survey of Japan, National Institute of Advanced Industrial Science and Technology, 1‐1‐1 Higashi, Tsukuba 305‐8567, Japan, [email protected]

Publisher: Seismological Society of America

First Online: 14 Jul 2017

Online ISSN: 1938-2057

Print ISSN: 0895-0695

Seismological Research Letters (2016) 87 (5): 1044–1049.

https://doi.org/10.1785/0220160107

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Preliminary Analysis of Strong Ground Motions in the Heavily Damaged Zone in Mashiki Town, Kumamoto, Japan, during the Mainshock of the 2016 Kumamoto Earthquake (⁠ $M_{w}$ 7.0) Observed by a Dense Seismic Array

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Preliminary Analysis of Strong Ground Motions in the Heavily Damaged Zone in Mashiki Town, Kumamoto, Japan, during the Mainshock of the 2016 Kumamoto Earthquake (⁠ $M_{w}$ 7.0) Observed by a Dense Seismic Array