Coseismic fault rupture at the trench axis during the 2011 Tohoku-oki earthquake

被引:0
|
作者
Shuichi Kodaira
Tetsuo No
Yasuyuki Nakamura
Toshiya Fujiwara
Yuka Kaiho
Seiichi Miura
Narumi Takahashi
Yoshiyuki Kaneda
Asahiko Taira
机构
[1] Institute for Research on Earth Evolution,
[2] Japan Agency for Marine-Earth Science and Technology,undefined
[3] Earthquake and Tsunami Research Project for Disaster Prevention,undefined
[4] Japan Agency for Marine-Earth Science and Technology,undefined
[5] Japan Agency for Marine-Earth Science and Technology,undefined
关键词
D O I
10.1038/ngeo1547
中图分类号
学科分类号
摘要
Subduction zone models often assume that the shallowest part of the plate interface slips aseismically. Images of the subduction trench next to the Tohoku-oki epicentre, captured using seismic reflection data 11 days after the 2011 earthquake, reveal deformation structures in sediments next to the trench, indicating that fault slip did reach the sea floor.
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页码:646 / 650
页数:4
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