Abstract: Shallow Slow Earthquake Activity from the Nankai Trough to the Ryukyu Trench Revealed by Long-term Ocean Bottom Seismological Observation (2017 AGU Fall Meeting)

Shallow Slow Earthquake Activity from the Nankai Trough to the Ryukyu Trench Revealed by Long-term Ocean Bottom Seismological Observation

Yusuke Yamashita¹, Masanao Shinohara², Hiroshi Yakiwara³, Tomoaki Yamada⁴, Saki Watanabe⁵, Kazuo Nakahigashi⁶, Hajime Shiobara⁴, Kimihiro Mochizuki⁴, Takuto Maeda⁴ and Kazushige Obara⁷, (1)Disaster Prevention Research Institute, Kyoto University, Kyoto, Japan, (2)National Research Institute for Earth Science and Disaster Resilience/Earthquake Research Institute, The University of Tokyo, Tokyo, Japan, (3)Kagoshima University, Kagoshima, Japan, (4)Earthquake Research Institute, The University of Tokyo, Tokyo, Japan, (5)Kyushu University, Fukuoka, Japan, (6)Tokyo University of Marine Science and Technology, Department of Marine Resources and Energy, Tokyo, Japan, (7)The University of Tokyo, Earthquake Research Institute, Tokyo, Japan

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