日本地球惑星科学連合2021年大会

講演情報

[J] ポスター発表

セッション記号 S (固体地球科学) » S-CG 固体地球科学複合領域・一般

[S-CG49] 島弧の構造・進化・変形とプレート沈み込み作用

2021年6月4日(金) 17:15 〜 18:30 Ch.17

コンビーナ:石川 正弘(横浜国立大学大学院環境情報研究院)、篠原 雅尚(東京大学地震研究所)、松原 誠(防災科学技術研究所)、石山 達也(東京大学地震研究所)

17:15 〜 18:30

[SCG49-P05] Upper mantle structure beneath the Japan Sea revealed by repeating long-term seafloor seismic observations

*中東 和夫1、悪原 岳2、山田 知朗3、望月 公廣2、山下 裕亮4、塩原 肇2、篠原 雅尚2 (1.東京海洋大学、2.東京大学地震研究所、3.気象庁、4.京都大学防災研究所)

The Japan Sea, which has located between the Asian continent and the Japan Islands, is a back-arc basin in the northwestern Pacific Ocean. The Japan Sea is believed to have been formed by back-arc opening and numerous and various models have been proposed by many geophysical and geological studies to explain the formation and evolution. Many crustal structure surveys with ocean bottom seismometers (OBSs) have been performed to better understand the formation of the Japan Sea. Different types of crust have been found. The Japan Basin has an oceanic crust in the northeastern area. The Tsushima Basin has the crustal thickness approximately 15 km. The Kita-Yamato Trough, which splits the Yamato Rise into two parts, has the crustal thickness of about 12 km without high velocity layer (7.1 km/s) in the lower crust. In the Yamato Rise area, seismic crustal survey with OBSs has not been conducted, however, gravity data suggest that depth of Moho is about 24 km. To understand the formation of the crust and the evolution of the Japan Sea, it is necessary to determine the deep seismic structure. Regional tomography using the land station data did not have a sufficient resolution to image a deep structure beneath the sea area. To obtain the deep structure, observations of natural earthquakes within the sea area are essential. Therefore, we started the repeating long-term seismic observations using OBSs from 2013 to 2019. We apply travel-time tomography method to the regional earthquake arrival-data recorded by OBSs and land stations. In this presentation, we will report the P and S wave tomographic images beneath the Japan Sea.
This study was supported by “Integrated Research Project on Seismic and Tsunami Hazards around the Sea of Japan” conducted by the Ministry of Education, Culture, Sports, Science, and Technology (MEXT) of Japan.