Structure of the tsunamigenic plate boundary and low-frequency earthquakes in the southern Ryukyu Trench

Weakly coupled subduction zones may generate earthquakes that lead to tsunamis, but their structure and seismicity are poorly constrained with the Ryukyu subduction zone as one such example. Here, Arai et al. present seismological evidence from Ryukyu showing megathrust faults and low frequency eart...

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Autores principales:	Ryuta Arai, Tsutomu Takahashi, Shuichi Kodaira, Yuka Kaiho, Ayako Nakanishi, Gou Fujie, Yasuyuki Nakamura, Yojiro Yamamoto, Yasushi Ishihara, Seiichi Miura, Yoshiyuki Kaneda
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2016
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/31071945837246a0a3a7598609e03072
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spelling	oai:doaj.org-article:31071945837246a0a3a7598609e030722021-12-02T16:57:18ZStructure of the tsunamigenic plate boundary and low-frequency earthquakes in the southern Ryukyu Trench10.1038/ncomms122552041-1723https://doaj.org/article/31071945837246a0a3a7598609e030722016-07-01T00:00:00Zhttps://doi.org/10.1038/ncomms12255https://doaj.org/toc/2041-1723Weakly coupled subduction zones may generate earthquakes that lead to tsunamis, but their structure and seismicity are poorly constrained with the Ryukyu subduction zone as one such example. Here, Arai et al. present seismological evidence from Ryukyu showing megathrust faults and low frequency earthquakes.Ryuta AraiTsutomu TakahashiShuichi KodairaYuka KaihoAyako NakanishiGou FujieYasuyuki NakamuraYojiro YamamotoYasushi IshiharaSeiichi MiuraYoshiyuki KanedaNature PortfolioarticleScienceQENNature Communications, Vol 7, Iss 1, Pp 1-7 (2016)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q Ryuta Arai Tsutomu Takahashi Shuichi Kodaira Yuka Kaiho Ayako Nakanishi Gou Fujie Yasuyuki Nakamura Yojiro Yamamoto Yasushi Ishihara Seiichi Miura Yoshiyuki Kaneda Structure of the tsunamigenic plate boundary and low-frequency earthquakes in the southern Ryukyu Trench
description	Weakly coupled subduction zones may generate earthquakes that lead to tsunamis, but their structure and seismicity are poorly constrained with the Ryukyu subduction zone as one such example. Here, Arai et al. present seismological evidence from Ryukyu showing megathrust faults and low frequency earthquakes.
format	article
author	Ryuta Arai Tsutomu Takahashi Shuichi Kodaira Yuka Kaiho Ayako Nakanishi Gou Fujie Yasuyuki Nakamura Yojiro Yamamoto Yasushi Ishihara Seiichi Miura Yoshiyuki Kaneda
author_facet	Ryuta Arai Tsutomu Takahashi Shuichi Kodaira Yuka Kaiho Ayako Nakanishi Gou Fujie Yasuyuki Nakamura Yojiro Yamamoto Yasushi Ishihara Seiichi Miura Yoshiyuki Kaneda
author_sort	Ryuta Arai
title	Structure of the tsunamigenic plate boundary and low-frequency earthquakes in the southern Ryukyu Trench
title_short	Structure of the tsunamigenic plate boundary and low-frequency earthquakes in the southern Ryukyu Trench
title_full	Structure of the tsunamigenic plate boundary and low-frequency earthquakes in the southern Ryukyu Trench
title_fullStr	Structure of the tsunamigenic plate boundary and low-frequency earthquakes in the southern Ryukyu Trench
title_full_unstemmed	Structure of the tsunamigenic plate boundary and low-frequency earthquakes in the southern Ryukyu Trench
title_sort	structure of the tsunamigenic plate boundary and low-frequency earthquakes in the southern ryukyu trench
publisher	Nature Portfolio
publishDate	2016
url	https://doaj.org/article/31071945837246a0a3a7598609e03072
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Structure of the tsunamigenic plate boundary and low-frequency earthquakes in the southern Ryukyu Trench

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