Session Details
[S08P]PM-P
Mon. Oct 24, 2022 3:30 PM - 6:00 PM JST
Mon. Oct 24, 2022 6:30 AM - 9:00 AM UTC
Mon. Oct 24, 2022 6:30 AM - 9:00 AM UTC
ROOM P-2 10th floor (Conference Room 1010-1070)
[S08P-01]Stress field and slip tendency analysis for the 2016 Mw7.8 Kaikōura earthquake, New Zealand
*Tomomi Okada1, Miu Matsuno1, Ayaka Tagami1, Satoshi Matsumoto2, Yuta Kawamura2, Yoshihisa Iio3, Tadashi Sato1, Takashi Nakayama1, Satoshi Hirahara1, Stephen Bannister4, John Ristau4, Martha K Savage5, Clifford H Thurber6, Richard H Sibson7 (1. Research Center for Prediction of Earthquakes and Volcanic Eruptions, Graduate School of Science, Tohoku University, 2. Institute of Seismology and Volcanology, Faculty of Science, Kyushu University, 3. Disaster Prevention Research Institute, Kyoto University, 4. GNS Science, New Zealand, 5. Victoria University of Wellington, New Zealand, 6. University of Wisconsin - Madison, United States of America, 7. University of Otago, New Zealand)
[S08P-02]Source process analysis of the 2004 off Kii peninsula earthquake from using sparse observation network and Green functions based on a three-dimensional structure
*TAKAHITO NISHIMIYA1 (1. Second Laboratory, Department of Seismology and Tsunami Research, Meteorological Research Institute, Japan Meteorological Agency)
[S08P-03]Commonality and diversity of ruptures occurring at the same asperity: the 2015 Mw6.8 Miyagi-Oki earthquake and Mw6.0-6.4 quasi-repeating earthquakes
*Keisuke YOSHIDA1 (1. Research Center for Prediction of Earthquakes and Volcanic Eruptions, Tohoku University)
[S08P-04]Relationship Between Variations in Source Duration and Occurrence Areas of Earthquakes
*Goki Irie1, Junichi Nakajima1 (1. Tokyo Institute of Technology)
[S08P-05]Do deep low frequency earthquakes have the similar rupture growth process to ordinary earthquakes?
*Genki OIKAWA1, Naofumi Aso1 (1. Tokyo Institute of Technology)
[S08P-06]What Actually is the Vertical Shock Verbally Reported for Shallow Earthquakes?
*Koji UENISHI1 (1. Univ. of Tokyo)
[S08P-07]Outline and radiation efficiency of stochastic source time functions
*Shiro HIRANO1 (1. Ritsumeikan Univ.)
[S08P-08]On shear localization by thermo-chemical pressurization and following destabilization and migration of the shear-localized zone
*Shunya KANEKI1, Hiroyuki Noda1 (1. Kyoto University, DPRI)
[S08P-09]The earthquake interoccurrence time distribution in sheared granular model
*Ryunosuke Sakamoto1, Takahiro Hatano1 (1. Osaka University)
[S08P-10]Numerical experiments using a friction law both for fast and slow sliding
*Takane HORI1, Hideo Aochi2 (1. Japan Agency for Marine-Earth Science and Technology, 2. BRGM (French Geological Survey))
[S08P-11]Investigation of earthquake source scaling laws using dynamic rupture simulations with a hierarchical patch structure
*Kazuki Masuda1, Yoshihiro Kaneko1 (1. Kyoto University)
[S08P-12]Dynamic simulations of coseismic slickenlines on non-planar and rough faults
*Takumi Aoki1, Yoshihiro Kaneko1, Jesse Kearse2 (1. Kyoto University, 2. Victoria University of Wellington)
[S08P-13]Investigation of multi-segment earthquake on the Median Tectonic Line active fault zone based on dynamic rupture simulation (Part 2)
*Yuko KASE1, Yumi URATA1 (1. Geological Survey of Japan, AIST)
[S08P-14]Why do Gutenberg-Richter b-values decrease with time prior to large earthquakes? Insights from rate-and-state earthquake cycle simulations with frictional heterogeneities
*Ryo Ito1, Yoshihiro Kaneko1 (1. Kyoto University)
[S08P-15]Numerically reproduced segments of short-term slow slip events in the Nankai region
*Takanori MATSUZAWA1, Bunichiro Shibazaki2 (1. National Reserach Institute for Earth Science and Disaster Resilience, 2. Building Research Institute)
[S08P-16]Impact of Kuroshio meanders on a stationary slow slip event and local seafloor level change around the Nankai Trough
*Keisuke ARIYOSHI1, Akira Nagano1, Takuya Hasegawa2, Takeshi Iinuma1, Masaru Nakano1, Demian Michael Saffer4, Hiroyuki Matsumoto1, Shuichiro Yada1, Eiichiro Araki1, Narumi Takahashi3, Takane Hori1, Shuichi Kodaira1 (1. JAMSTEC, 2. Faculty of Environmental Earth Science, Hokkaido University (now at Japan Meteorological Agency), 3. National Research Institute for Earth Science and Disaster Resilience, 4. University of Texas, Austin)
[S08P-17]A possible relation between Reidel shear band and rate- and state-dependent friction parameters
*Eiichi FUKUYAMA1,2, Futoshi Yamashita2, Sumire Maeda2, Akihiro Shimoda1, Shun Watanabe1 (1. Kyoto University, 2. NIED)