How did the 2011 off the Pacific coast of Tohoku Earthquake start and grow? The role of a conditionally stable area
スポンサーリンク
概要
- 論文の詳細を見る
- Terra Scientific Pub. Coの論文
- 2011-07-01
著者
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IIO Yoshihisa
Research Center for Earthquake Prediction, Disaster Prevention Research Institute, Kyoto University
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Iio Yoshihisa
Research Center For Earthquake Prediction Disaster Prevention Research Institute Kyoto University
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MITSUI Yuta
Research Center for Earthquake Prediction, Disaster Prevention Research Institute, Kyoto University
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Mitsui Yuta
Research Center For Earthquake Prediction Disaster Prevention Research Institute Kyoto University
関連論文
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- A comprehensive model of the deformation process in the Nagamachi-Rifu Fault Zone
- What controls the occurrence of shallow intraplate earthquakes?
- Origin of the concentrated deformation zone in the Japanese Islands and stress accumulation process of intraplate earthquakes
- How did the 2011 off the Pacific coast of Tohoku Earthquake start and grow? The role of a conditionally stable area
- Imaging of S-wave reflectors in and around the hypocentral area of the 2004 mid Niigata Prefecture Earthquake (M6.8)
- Three dimensional velocity structure around aftershock area of the 2004 mid Niigata prefecture earthquake (M6.8) by the Double-Difference tomography
- Modeling slip processes at the deeper part of the seismogenic zone using a constitutive law combining friction and flow laws