Lithospheric thickness and upper-mantle deformation beneath the NE Tibetan Plateau inferred from S receiver functions and SKS splitting measurements

Geophysical Journal International

Volumn 191, Issue 3, 2012, Pages 1285-1294

  Zhang, Hongshuang ^a,b   Teng, Jiwen ^b   Tian, Xiaobo ^b   Zhang, Zhongjie ^b   Gao, Rui ^a   Liu, Jiaqi ^b  

^a INSTITUTE OF GEOLOGY   (China)

^b INSTITUTE OF GEOLOGY AND GEOPHYSICS   (China)

Author keywords

Body waves; Continental tectonics: extensional; Dynamics of lithosphere and mantle; Seismic anisotropy

Indexed keywords

BODY WAVES; CONTINENTAL TECTONICS; DELAY TIME; EAST KUNLUN; GANSU PROVINCE; KUNLUN FAULT; LITHOSPHERE-ASTHENOSPHERE BOUNDARY; LITHOSPHERIC THICKNESS; QAIDAM BASIN; S-RECEIVER FUNCTIONS; SEISMIC ANISOTROPY; SEISMOGRAPH NETWORKS; SHEAR WAVE SPLITTING; SPLITTING MEASUREMENTS; TELESEISMIC; TIBETAN PLATEAU; UPPERMOST MANTLE;

SHEAR WAVES; STRUCTURAL GEOLOGY; TECTONICS;

DEFORMATION;

BODY WAVE; CRUSTAL THICKNESS; DEFORMATION; EXTENSIONAL TECTONICS; GEODYNAMICS; LITHOSPHERIC STRUCTURE; OROGENY; S-WAVE; SEISMIC ANISOTROPY; SEISMIC DATA; SEISMOGRAPH; SEISMOTECTONICS; SUTURE ZONE; TELESEISMIC WAVE; UPPER MANTLE; WAVE SPLITTING;

CHINA; GANSU; QAIDAM BASIN; QINGHAI; QINGHAI-XIZANG PLATEAU; SONGPAN-GANZI BASIN;

EID: 84869096997     PISSN: 0956540X     EISSN: 1365246X     Source Type: Journal    
DOI: 10.1111/j.1365-246X.2012.05667.x     Document Type: Article

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