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《Chinese Journal of Geophysics》 2002-05
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HIGH RESOLUTION SURFACE WAVE TOMOGRAPHY IN EAST ASIA AND WEST PACIFIC MARGINAL SEAS

ZHU JIE SHOU\ CAO JIA MIN\ CAI XUE LIN\ YAN ZHONG QIONG\ CAO XIAO LIN (Department of Geophysics, Chengdu University of Technology, Chengdu 610059, China)  
This paper deals with the high resolution surface wave tomography in East Asia and West Pacific marginal seas (60°-160°E,20°S-60°N). Twelve thousands long period digital seismic waveforms from 650 events (7.0≥ M ≥5.0) recorded at 58 digital seismic stations from CDSN, GSN, GDSN and GEOSCOPE network in Eurasia and west Pacific regions were used in this paper. Four thousands and one hundred accurate surface dispersion curves with periods ranging 8 to 250 seconds were selected and employed for inversion. The high resolution 3 D shear wave velocity images in this area was constructed by inversion of both dispersion and waveform and show a notable lateral variation in the crust and upper mantle.\;The images of S wave velocity indicate that from the upper crust to the depth of 70km, the high velocity is displayed in the region of eastern part of East Asia and West Pacific marginal seas, in contrast, extremely low velocity is in the Qinghai Xizang plateau and its surrounding areas. There exists a boundary of velocity decrease along the Mountain belt from Da Xingganling to Taihangshan, Wulinshan, which coincides with the gravity gradient belt in NNE-SSW trend in East China. The low velocity anomaly chain is located along the convergence belt of Tethys from Mediterranean Sea, Turkey, Iran, Himalayan orogens, Burma, Indonesian Islands.\;The evolution and geodynamic process is so different between the eastern part and western part of the East Asia and West Pacific marginal seas by the boundary of longitude 110°E. The western part is the thickening convergent lithosphere caused by Indian subcontinent collided with the Eurasian continent, and the eastern part is disassembly causing the lithosphere thinning and extension arising from intrusion of asthenospheric material.
【Fund】: 国家自然科学基金重点项目 ( 49734 150 );; 国土资源部专项计划项目 ( 2 0 0 0 10 10 );; 国家重点基础研究发展规划项目 (G19980 4 0 80 1);; 油气藏地质及开发工程国家重点实验室资助项目
【CateGory Index】: P315.2
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4 Liang Zhao and Tianyu Zheng Seismological Laboratory(SKL-LE),Institute of Geology and Geophysics,Chinese Academy of Sciences,China.;Complex upper-mantle deformation beneath the North China Craton:implications for lithospheric thinning[A];[C];2008
5 TIAN You~(1,2),ZHAO Da-Peng~2,SUN Rou-Mei~1,TENG Ji-Wen~(1,3) 1 Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China 2 Research Center for Prediction of Earthquakes and Volcanic Eruptions,Tohoku University,Sendai 980 - 8578,Japan 3 Jilin University,Changchun 130026,China;The 1992 Landers earthquake:Effect of crustal heterogeneity on earthquake generation[A];[C];2008
6 ZHANG XueMei~(1+),SUN RuoMei~1 &TENG JiWen~(1,2) 1 Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China; 2 College of Geo-exploration Science and Technology,Jilin University,Changchun 130026,China;Study on crustal,lithospheric and asthenospheric thickness beneath the Qinghai-Tibet Plateau and its adjacent areas[A];[C];2008
7 SU BenXun~1,ZHANG HongFu~(1**),WANG QiaoYun~2,SUN He~1,XIAO Yan~1 and YING JiFeng~1 1.State Key Laboratory of Lithospheric Evolution,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China 2.State Key Laboratory of Ore Deposit Geochemistry,Institute of Geochemistry,Chinese Academy of Sciences,Guiyang 550002,China;Spinel-garnet phase transition zone of Cenozoic lithospheric mantle beneath the eastern China and western Qinling and its T-P condition[A];[C];2008
8 Mingguo Zhai~(a,b,d,*),Qicheng Fan~c,Hongfu Zhang~(a,d),Jianli Sui~a,Ji'an Shao~e a Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing,100029,China b Key Laboratory of Mineral Resources.Chinese Academy of Sciences,Beijing,100029,China c Institute of Geology,Chinese Seismological Bureau.Beijing,100029,China d State Key Laboratory of Lithosphere Tectonic Evolution,Beijing,100029,China c School of Earth and Space Sciences,Peking University,Beijing,100871,China;Lower crustal processes leading to Mesozoic lithospheric thinning beneath eastern North China:Underplating,replacement and delamination[A];[C];2008
9 H.-F.ZHANG State Key Laboratory of Lithospheric Evolution,Institute of Geology and Geophysics, Chinese Academy of Sciences,PO Box 9825,Beijing 100029,China;Temporal and spatial distribution of Mesozoic mafic magmatism in the North China Craton and implications for secular lithospheric evolution[A];[C];2008
10 ZHANG Qi,PAN GuoQiang,LI ChengDong,JIN Weijun and JIA XiuQin 1.Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029 2.Department of Earth Sciences,Nanjing University,Nanjing 210093 3.Tianjin Institute of Geology and Mineral Resources,Tianjin 300170 4.Institute of High Energy Physics,Chinese Academy of Sciences,Beijing 100039;Are discrimination diagrams always indicative of correct tectonic settings of granites?-some crucial questions on granite study(3)[A];[C];2008
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