固体地球科学(S) | |||
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セッション小記号 | 固体地球科学複合領域・一般(CG) | ||
セッションID | S-CG50 | ||
タイトル | 和文 | Earthquakes, Tsunamis, Seismotectonics, and Hazard Potential of the Ryukyu Trench and Okinawa Trough | |
英文 | Earthquakes, Tsunamis, Seismotectonics, and Hazard Potential of the Ryukyu Trench and Okinawa Trough | ||
タイトル短縮名 | 和文 | Ryukyu Trench and Okinawa Trough | |
英文 | Ryukyu Trench and Okinawa Trough | ||
代表コンビーナ | 氏名 | 和文 | 佐竹 健治 |
英文 | Kenji Satake | ||
所属 | 和文 | 国立中央大学(台湾) | |
英文 | Dept. Earth Sciences, National Central University, Taiwan | ||
共同コンビーナ 1 | 氏名 | 和文 | 中村 衛 |
英文 | Mamoru Nakamura | ||
所属 | 和文 | 琉球大学理学部 | |
英文 | Faculty of Science, University of the Ryukyus | ||
共同コンビーナ 2 | 氏名 | 和文 | CHANG PINGYU |
英文 | CHANG PINGYU | ||
所属 | 和文 | National Central University, Taiwan | |
英文 | National Central University, Taiwan | ||
共同コンビーナ 3 | 氏名 | 和文 | J. Bruce H. Shyu |
英文 | J. Bruce H. Shyu | ||
所属 | 和文 | National Taiwan University | |
英文 | National Taiwan University | ||
発表言語 | E | ||
スコープ | 和文 |
Along the Ryukyu trench between Kyushu and Taiwan, the Philippine Sea plate subducts beneath the Eurasian Plate with a rate of approximately 8 cm/year. Unlike the neighboring Nankai Trough, the history of great interplate earthquakes is not well known, except for the enigmatic 1771 Meiwa earthquake, which caused more than 10,000 casualties due to tsunami. The Hualien earthquake on April 3, 2024 (M 7.4) originated from this plate boundary, causing the worst earthquake damage to Taiwan since the 1999 Chi-chi earthquake. The Hualien earthquake also prompted a tsunami warning in Ryukyu Islands, Japan. The Okinawa Trough, which is located on the northwest side of the Ryukyu Arc, is currently in the early stages of back-arc rifting. Associated with the rifting, seismic swarm activity and hydrothermal activity are also active within the trough. However, the mechanism of the Okinawa Trough's extension is still unknown. The geodetic measurements on the Ryukyu islands indicate that the plate coupling is very weak, while recent offshore geodetic measurements indicate coupled patches along the megathrust. Slow earthquakes have been observed along the Ryukyu trench. In order to exchange current knowledge on the Ryukyu trench and stimulate further collaboration between Taiwan and Japan, we propose a joint session between Chinese Geoscience Union in Taiwan (TCGU) and JpGU. This session solicits recent studies on earthquakes, tsunamis or seismotectonics. Possible topics include, but not limited to, studies of the 2024 Hualien earthquake and its tsunami, recent geophysical observations of slow or regular earthquakes, studies of past earthquakes in the region, Probabilistic Seismic Hazard Assessments of the region. |
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英文 |
Along the Ryukyu trench between Kyushu and Taiwan, the Philippine Sea plate subducts beneath the Eurasian Plate with a rate of approximately 8 cm/year. Unlike the neighboring Nankai Trough, the history of great interplate earthquakes is not well known, except for the enigmatic 1771 Meiwa earthquake, which caused more than 10,000 casualties due to tsunami. The Hualien earthquake on April 3, 2024 (M 7.4) originated from this plate boundary, causing the worst earthquake damage to Taiwan since the 1999 Chi-chi earthquake. The Hualien earthquake also prompted a tsunami warning in Ryukyu Islands, Japan. The Okinawa Trough, which is located on the northwest side of the Ryukyu Arc, is currently in the early stages of back-arc rifting. Associated with the rifting, seismic swarm activity and hydrothermal activity are also active within the trough. However, the mechanism of the Okinawa Trough's extension is still unknown. The geodetic measurements on the Ryukyu islands indicate that the plate coupling is very weak, while recent offshore geodetic measurements indicate coupled patches along the megathrust. Slow earthquakes have been observed along the Ryukyu trench. In order to exchange current knowledge on the Ryukyu trench and stimulate further collaboration between Taiwan and Japan, we propose a joint session between Chinese Geoscience Union in Taiwan (TCGU) and JpGU. This session solicits recent studies on earthquakes, tsunamis or seismotectonics. Possible topics include, but not limited to, studies of the 2024 Hualien earthquake and its tsunami, recent geophysical observations of slow or regular earthquakes, studies of past earthquakes in the region, Probabilistic Seismic Hazard Assessments of the region. |
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発表方法 | 口頭および(または)ポスターセッション | ||
ジョイントセッション | CGU | ||
招待講演 |
Ma Kuo-Fong (Institute of Geophysics, National Central University, Taiwan, ROC) 藤井 雄士郎 (国立研究開発法人 建築研究所 国際地震工学センター) 中村 衛 (琉球大学理学部) 生田 領野 (静岡大学理学部) Cheng-Hung CHEN (Department of Geosciences, National Taiwan University) Pei-Ru Jian (Department of Geosciences, National Taiwan University) |
時間 | 講演番号 | タイトル | 発表者 |
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口頭発表 5月28日 PM1 | |||
13:45 - 14:00 | SCG50-01 | Earthquakes, Tsunamis, Seismotectonics, and Hazard Potential of the Ryukyu Trench and Okinawa Trough - Introduction | 佐竹 健治 |
14:00 - 14:15 | SCG50-02 | A Comparative Analysis of the November 14, 1986, and April 2, 2024, Hualien, Taiwan earthquakes: Seismic Source Characteristics and Regional Impacts | Ma Kuo-Fong |
14:15 - 14:30 | SCG50-03 | Spatiotemporal Patterns of the April 2, 2024, Hualien Earthquake Sequence and Finite Fault Solutions of Significant Aftershocks | Yopi Ruben Serhalawan |
14:30 - 14:45 | SCG50-04 | 台湾の花蓮市付近で2024年4月3日に発生した地震(M7.4)の津波シミュレーション | 藤井 雄士郎 |
14:45 - 15:00 | SCG50-05 | Source mechanism and early warning of volcanic tsunamis | Tony Song |
15:00 - 15:15 | SCG50-06 | Develop new numerical method CGM to simulate landslides and enhance the description of turbidity suspension phenomena | Cheng-Hao Yeh |
口頭発表 5月28日 PM2 | |||
15:30 - 15:45 | SCG50-07 | Decadal-Scale Changes in Very Low-Frequency Earthquake Activity in the Southwestern Ryukyu Trench | 中村 衛 |
15:45 - 16:00 | SCG50-08 | GNSS-Aにより明らかになった琉球海溝南端部のプレート間カップリングの欠如 | 生田 領野 |
16:00 - 16:15 | SCG50-09 | The Offshore Seismogenic Structure Database in Northeast Taiwan | Cheng-Hung CHEN |
16:15 - 16:30 | SCG50-10 | The New Ryukyu Area CMT (RACMT) Catalog: Implications for Ryukyu Subduction Zone Rupture Behavior | Pei-Ru Jian |
16:30 - 16:45 | SCG50-11 | Long-term vertical deformations in the Ryukyu subduction zone, Japan | Sophie Debaecker |
16:45 - 17:00 | SCG50-12 | Analysis of Subsurface Fault Systems Using Audio-Magnetotelluric Surveys in the Western Ilan Plain , the tip of the extension of Okinawa Trough | CHANG PINGYU |
講演番号 | タイトル | 発表者 |
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ポスター発表 5月28日 PM3 | ||
SCG50-P01 |
Matched filter 法を用いた沖縄トラフにおける 群発地震の時空間変動の解析 |
安部 祐志 |
SCG50-P02 | 南西諸島前弧域における付加体を含む地盤構造モデルの改良 | 小松 正直 |
SCG50-P03 | Reconstructing relative sea-level changes on Kikaijima Island from coral microatolls: Implications for megathrust earthquake potential along the Ryukyu Trench | 小森 純希 |
SCG50-P04 | Coupled Dynamics of Internal Waves and Submarine Landslides in the Formation of Nepheloid Layers | Che-Han Chang |