| 东亚及西太平洋边缘海高分辨率面波层析成像 |
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| 引用本文： | 朱介寿,曹家敏,蔡学林,严忠琼,曹小林.东亚及西太平洋边缘海高分辨率面波层析成像[J].地球物理学报,2002,45(5):646-664. |
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| 作者姓名： | 朱介寿 曹家敏 蔡学林 严忠琼 曹小林 |
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| 作者单位： | 成都理工大学地球物理系,成都,610059 |
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| 基金项目： | 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 |
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| 摘 要： | 根据欧亚大陆及西太平洋地区58个数字地震台站约12000个长周期波形记录,挑选出4100条面波大圆传播路径,采用面波频散及波形拟合反演方法,对东亚及西太平洋边缘海地区(60°E-160°E,20°S-60°N)的地壳上地幔进行了高分辨率三维S波速度成像. 结果表明,从上地壳到70km深,在东亚东部及西太平洋边缘海地区为高速分布,西部以青藏高原为中心呈极低速分布. 自地中海经土耳其、伊朗、喜马拉雅山到缅甸、印尼群岛的特提斯汇聚碰撞带,显示为低速异常链. 从85km至250km深,在东亚东部及西太平洋边缘海,自北向南显示出一条巨型低速异常带,西部地区为高速异常分布.以东经110°E为界,东西两部分岩石圈、软流圈的结构与深部动力过程有着巨大的差异. 此界线以西主要是印度板块与欧亚板块碰撞引起的岩石圈汇聚增厚区,东部则主要是由于软流圈上涌(地幔热物质上升)引起的岩石圈拉张减薄区.
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| 关 键 词： | 高分辨率面波三维层析成像 东亚及西太平洋边缘海巨型低速带 岩石圈软流圈结构及动力学 |
| 文章编号： | 0001-5733(2002)05-0646-19 |
| 收稿时间： | 2001-06-27 |
HIGH RESOLUTION SURFACE WAVE TOMOGRAPHY IN EAST ASIA AND WEST PACIFIC MARGINAL SEAS |
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| ZHU JIE,SHOU\ CAO JIA,MIN\ CAI XUE,LIN\ YAN ZHONG,QIONG\ CAO XIAO,LIN.HIGH RESOLUTION SURFACE WAVE TOMOGRAPHY IN EAST ASIA AND WEST PACIFIC MARGINAL SEAS[J].Chinese Journal of Geophysics,2002,45(5):646-664. |
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| Authors: | ZHU JIE SHOU\ CAO JIA MIN\ CAI XUE LIN\ YAN ZHONG QIONG\ CAO XIAO LIN |
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| Institution: | Department of Geophysics, Chengdu University of Technology, Chengdu 610059, China |
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| Abstract: | 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. |
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| Keywords: | East Asia and West Pacific marginal seas Surface wave 3 D tomography The giant low velocity zone and rifting system in East Asia and West Pacific marginal sea The structure and dynamics of lithosphere and asthenosphere |
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