JpGU-AGU Joint Meeting 2017

講演情報

[EJ] ポスター発表

セッション記号 S (固体地球科学) » S-IT 地球内部科学・地球惑星テクトニクス

[S-IT32] [EJ] Recent earthquakes and deep structure of the Earth in and around Tibetan Plateau

2017年5月24日(水) 15:30 〜 17:00 ポスター会場 (国際展示場 7ホール)

コンビーナ:白 玲(ITP Institute of Tibetan Plateau Research, Chinese Academy of Sciences)、Mori James(京都大学防災研究所地震防災研究部門)、佐藤 比呂志(東京大学地震研究所地震予知研究センター)、石川 有三(国立研究開発法人 産業技術研究所 活断層・火山研究部門)

[SIT32-P02] Subducting continental lower crust and crustal thickness variations in the intermediate seismic zone of Pamir-Hindu Kush from Moho underside reflection pmP

Hangqi He1、*Xiaobo He1 (1.Dept. of Marine Sciences, Zhejiang University)

キーワード:Moho, Intermediate earthquake, Pamir-Hindu Kush, Lower crust, Crustal thickness

The Pamir - Hindu Kush region is an orogenic belt presenting two continental converging subduction zones where the Indian and Asian plates collide. Understanding of the regional tectonic history, however, has been hampered due to limited seismological investigations. In this study, we use the Moho underside reflection pmP phases to constrain the crustal thickness variations in the intermediate seismic zone (36-37°N, 69-72°E). The events characterized by focal depth deeper than 100 km and magnitude greater than 5.8 (Mw) are selected. The crustal thickness is determined by identifying depth phase pP along with the Moho underside reflection pmP. The measured thickness in this study varies spatially from 58.1 to 76.2 km, with some uncertainty most likely resulting from the estimation of the average velocity of P-wave (~6.21 km/s) in the crust. The strong Moho variation implies a large structural deformation of the crust, reflecting a complex collision-related mountain building history. We also detect two strong reflections from deep interfaces down to ~97 km below the southernmost Pamir. According to our direct observations and waveform modeling, we further explain the two reflections are perhaps a result of underplating of the subducted Asian lower crust below this region. Our observations here will be complementary to other seismic results such as receiver functions.