Author
Listed:
- Ryuta Arai
(Research and Development Center for Earthquake and Tsunami, Japan Agency for Marine-Earth Science and Technology)
- Tsutomu Takahashi
(Research and Development Center for Earthquake and Tsunami, Japan Agency for Marine-Earth Science and Technology)
- Shuichi Kodaira
(Research and Development Center for Earthquake and Tsunami, Japan Agency for Marine-Earth Science and Technology)
- Yuka Kaiho
(Research and Development Center for Earthquake and Tsunami, Japan Agency for Marine-Earth Science and Technology)
- Ayako Nakanishi
(Research and Development Center for Earthquake and Tsunami, Japan Agency for Marine-Earth Science and Technology)
- Gou Fujie
(Research and Development Center for Earthquake and Tsunami, Japan Agency for Marine-Earth Science and Technology)
- Yasuyuki Nakamura
(Research and Development Center for Earthquake and Tsunami, Japan Agency for Marine-Earth Science and Technology)
- Yojiro Yamamoto
(Research and Development Center for Earthquake and Tsunami, Japan Agency for Marine-Earth Science and Technology)
- Yasushi Ishihara
(Research and Development Center for Earthquake and Tsunami, Japan Agency for Marine-Earth Science and Technology)
- Seiichi Miura
(Research and Development Center for Earthquake and Tsunami, Japan Agency for Marine-Earth Science and Technology)
- Yoshiyuki Kaneda
(Institute of Education, Research and Regional Cooperation for Crisis Management Shikoku, Kagawa University)
Abstract
It has been recognized that even weakly coupled subduction zones may cause large interplate earthquakes leading to destructive tsunamis. The Ryukyu Trench is one of the best fields to study this phenomenon, since various slow earthquakes and tsunamis have occurred; yet the fault structure and seismic activity there are poorly constrained. Here we present seismological evidence from marine observation for megathrust faults and low-frequency earthquakes (LFEs). On the basis of passive observation we find LFEs occur at 15–18 km depths along the plate interface and their distribution seems to bridge the gap between the shallow tsunamigenic zone and the deep slow slip region. This suggests that the southern Ryukyu Trench is dominated by slow earthquakes at any depths and lacks a typical locked zone. The plate interface is overlaid by a low-velocity wedge and is accompanied by polarity reversals of seismic reflections, indicating fluids exist at various depths along the plate interface.
Suggested Citation
Ryuta Arai & Tsutomu Takahashi & Shuichi Kodaira & Yuka Kaiho & Ayako Nakanishi & Gou Fujie & Yasuyuki Nakamura & Yojiro Yamamoto & Yasushi Ishihara & Seiichi Miura & Yoshiyuki Kaneda, 2016.
"Structure of the tsunamigenic plate boundary and low-frequency earthquakes in the southern Ryukyu Trench,"
Nature Communications, Nature, vol. 7(1), pages 1-7, November.
Handle:
RePEc:nat:natcom:v:7:y:2016:i:1:d:10.1038_ncomms12255
DOI: 10.1038/ncomms12255
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