Crustal structure of northeastern margin of the Tibetan Plateau by receiver function inversion

查看全文 作　　者：LIU [1,2]QiMin;ZHAO [1]JunMeng;LU [3]Fang;LIU [1]HongBing

机构地区：[1]Key Laboratory of Continental Collision and Plateau Uplift,Institute of Tibetan Plateau Research,Chinese Academy of Sciences;[2]University of Chinese Academy of Sciences;[3]Seismological Bureau of Hubei Province

出　　处：《Science China Earth Sciences》索引2014年第57卷第4期,共10页

基　　金：financially supported by National Natural Science Foundation of China(Grant No.40930317);CHINARE2012-02-02;Project SinoProbe-02-03;the NSFC Innovation Research Group Fund(Grant No.41021001) 摘　　要：Using seismic data of about one year recorded by 18 broadband stations of ASCENT project,we obtained 2547 receiver functions in the northeastern Tibetan Plateau.The Moho depths under 14 stations were calculated by applying the H-κ domain search algorithm.The Moho depths under the stations with lower signal-noise ratio(SNR) were estimated by the time delay of the PS conversion.Results show that the Moho depth varies in a range of ~40–60 km.The Moho near the Haiyuan fault is vague,and its depth is larger than those on its two sides.In the Qinling-Qilian Block,the Moho becomes shallower gradually from west to east.To the east of 105°E,the average depth of the Moho is 45 km,whereas the west is 50 km or even deeper.Combining our results with surface wave research,we suggest a boundary between the Qinling and the Qilian Mountains at around 105°E.S wave velocities beneath 15 stations have been obtained through a linear inversion by using Crust2.0 as an initial model,and the crustal thickness that was derived by H-κ domain search algorithm was also taken into account.The results are very similar to the results of previous active source studies.The resulting figure indicates that low velocity layers developed in the middle and lower crust beneath the transition zone of the Tibet Block and western Qinling,which may be related to regional faults and deep earth dynamics.The velocity of the middle and lower crust increases from the Songpan Block to the northeastern margin of Tibetan Plateau.Based on the velocity of the crust,the distribution of the low velocity zone and the composition of the curst(Poisson's ratio),we infer that the crust thickening results from the crust shortening along the direction of compression. 关键词：青藏高原东北缘地壳结构接收函数线性反演青藏高原东北部 TiAl基合金地球深部动力学时间延迟估计

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Crustal structure of northeastern margin of the Tibetan Plateau by receiver function inversion

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