In this paper we describe the earthquake geology of East Japan, based on a seismotectonic analysis of foreshocks and aftershocks for the 2011 Tohoku-oki Great Earthquake. The earthquake geology is defined by three compressional buttresses that are separated by channels dominated by extensional earthquakes. In the 2011 earthquake sequence, most activity occurred in the Tohoku-oki extensional channel. This is bounded by seismotectonic lineaments that run subparallel to the slip direction of thrust-fault earthquakes in the adjacent compressional buttresses, and to the slip direction of landward-dipping normal-fault aftershocks in the subducting Pacific plate. The northern bounding seismotectonic lineament of the Tohoku-oki extensional channel ...
The 2011 Tohoku earthquake (M 9.0) was much larger than typical interplate earthquakes (M<8) that oc...
AbstractThis paper gives an overview of the crustal deformation caused by “the 2011 off the Pacific ...
To better understand the earthquake dynamics of the Japan subduction zone, we investigated the later...
In this paper we describe the earthquake geology of East Japan, based on a seismotectonic analysis o...
International audienceThe 2011 Tohoku megathrust earthquake ruptured a vast region of the northeast ...
Abstract: A distinct difference of the earthquake activity in megathrust subduction zones is pointed...
The publication presents a review of the structure and seismotectonic features of the Pacific margin...
Fukao, Y. and Furumoto, M., 1975. Mechanism of large earthquakes along the eastern margin of the Jap...
The northern Japan (southern Kurile-Hokkaido-Honshu) region has a large history of large shallow ear...
The 11 March 2011 off the Pacific coast of Tohoku Earthquake (M_w 9.0) produced megathrust displacem...
The 11 March 2011 off the Pacific coast of Tohoku Earthquake (M_w 9.0) produced megathrust displacem...
The article presents results of tectonophysical methods applied to reconstruct tectonic stress field...
A distinct difference of the earthquake activity in megathrust subduction zones is pointed out, conc...
AbstractThis paper gives an overview of the crustal deformation caused by “the 2011 off the Pacific ...
To better understand the earthquake dynamics of the Japan subduction zone, we investigated the later...
The 2011 Tohoku earthquake (M 9.0) was much larger than typical interplate earthquakes (M<8) that oc...
AbstractThis paper gives an overview of the crustal deformation caused by “the 2011 off the Pacific ...
To better understand the earthquake dynamics of the Japan subduction zone, we investigated the later...
In this paper we describe the earthquake geology of East Japan, based on a seismotectonic analysis o...
International audienceThe 2011 Tohoku megathrust earthquake ruptured a vast region of the northeast ...
Abstract: A distinct difference of the earthquake activity in megathrust subduction zones is pointed...
The publication presents a review of the structure and seismotectonic features of the Pacific margin...
Fukao, Y. and Furumoto, M., 1975. Mechanism of large earthquakes along the eastern margin of the Jap...
The northern Japan (southern Kurile-Hokkaido-Honshu) region has a large history of large shallow ear...
The 11 March 2011 off the Pacific coast of Tohoku Earthquake (M_w 9.0) produced megathrust displacem...
The 11 March 2011 off the Pacific coast of Tohoku Earthquake (M_w 9.0) produced megathrust displacem...
The article presents results of tectonophysical methods applied to reconstruct tectonic stress field...
A distinct difference of the earthquake activity in megathrust subduction zones is pointed out, conc...
AbstractThis paper gives an overview of the crustal deformation caused by “the 2011 off the Pacific ...
To better understand the earthquake dynamics of the Japan subduction zone, we investigated the later...
The 2011 Tohoku earthquake (M 9.0) was much larger than typical interplate earthquakes (M<8) that oc...
AbstractThis paper gives an overview of the crustal deformation caused by “the 2011 off the Pacific ...
To better understand the earthquake dynamics of the Japan subduction zone, we investigated the later...