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Earthquake relocation and 3-dimensional crustal structure of P-wave velocity in cen-tral-western China
作者姓名:杨智娴  于湘伟  郑月军  陈运泰  倪晓晞  Winston CHAN
作者单位:Institute of Geophysics,China Seismological Bureau,Institute of Geophysics,China Seismological Bureau,Institute of Crustal Dynamics,China Seismological Bureau,Institute of Geophysics,China Seismological Bureau,Multimax,Inc.,MD 20774,USA,Multimax,Inc.,MD 20774,USA Beijing 100081,China,Beijing 100081,China,Beijing 100085,China,Beijing 100081,China
基金项目:Key Project Process Mechanism and Prediction of Geological Hazards (2001CB711005-1-3) and State Key Basic Research Project Mechanism and Prediction of Continental Earthquakes (G1998040702). sponsored by the Ministry of Science and Techno
摘    要:IntroductionUnderstandingthemechanismofcontinentalearthquakesisveryimportantforseismichaz-ardpreventionandearthquakeprediction.Themodernseismotectonictheoryandtheideaofearthquakepredictionaredevelopedmainlyfromthestudiesoninterplateearthquakes,whicharedifficulttoexplainthephenomenaofintraplateearthquakes,suchasthecontinentalearthquakesoccurredinChinesemainland.Whiletheinterplateearthquakesoccurredalongtheplatebounda-ries,theintraplateearthquakesdistributediffuselyintheinterioroftheplates.Thus…


Earthquake relocation and 3-dimensional crustal structure of P-wave velocity in central-western China
Winston CHAN.Earthquake relocation and 3-dimensional crustal structure of P-wave velocity in cen-tral-western China[J].Acta Seismologica Sinica(English Edition),2004,17(1):20-30.
Authors:Winston CHAN
Abstract:A simultaneous inversion of earthquake relocation and three-dimensional crustal structure of P-wave velocity in central-western China (21°N~36°N, 98°E~112°E) were performed in this paper. The crustal P-wave velocity model and earthquake relocation for this region are obtained using Pg and Sg phase readings of 9 988 earthquakes from 1992 to 1999 recorded at 193 seismic stations within central-western China by SPHYPIT90 and SPHREL3D90 programs. A lateral inhomogeneous structure of P-wave velocity in this region was obtained. Obvious contrast of P-wave velocities was revealed on both sides of active fault zones. Relocated epicenters of 6 459 events show clear lineation along active faults, which indicated a close correlation between seismicity and the active faults in this region. Focal depths of 82% relocated events ranged from 0 to 20 km, which is in good agreement with that from double-difference earthquake location algorithm.
Keywords:simultaneous inversion  3-D P-wave velocity structure  earthquake relocation  central-western China
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