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拉萨盆地曲水-夺底剖面大地电磁测深研究
引用本文:曹忠权,申旭辉,阎永利,马晓冰,袁国平,尤惠川,尹功明,滕春凯,谢平,美朵.拉萨盆地曲水-夺底剖面大地电磁测深研究[J].地球物理学报,2010,53(5):1173-1178.
作者姓名:曹忠权  申旭辉  阎永利  马晓冰  袁国平  尤惠川  尹功明  滕春凯  谢平  美朵
作者单位:1.中国地震局地质研究所拉萨地球物理国家野外科学观测研究站, 北京 100029;2.中国地震局地震预测研究所,北京 100036;3.中国科学院地质与地球物理研究所,北京 100029;4.浙江油田公司地质研究所,杭州 310013;5.西藏自治区地震局,拉萨 850000
基金项目:国家发改委城市活断层探测项目,国家973项目(2002CB412604)和国家自然科学基金项目(40774070)资助.
摘    要:通过对拉萨盆地曲水-夺底大地电磁测深剖面的研究,揭示了拉萨盆地深部地质构造特征.上地壳广泛分布花岗岩体,莫霍面深度大约70 km.壳内发育一个高导层,其顶界面埋深呈现南深北浅特点,厚度大约20~30 km,桑达附近存在一条深大断裂.

关 键 词:拉萨盆地  MT探测  壳幔结构  
收稿时间:2009-07-20
修稿时间:2010-01-11

The study of magnetotelluric sounding on Qushui-Duodi profile in Lhasa basin
CAO Zhong-Quan,SHEN Xu-Hui,YAN Yong-Li,MA Xiao-Bing,YUAN Guo-Ping,YOU Hui-Chuan,YIN Gong-Ming,TENG Chuan-Kai,XIE Pin,MEI Duo.The study of magnetotelluric sounding on Qushui-Duodi profile in Lhasa basin[J].Chinese Journal of Geophysics,2010,53(5):1173-1178.
Authors:CAO Zhong-Quan  SHEN Xu-Hui  YAN Yong-Li  MA Xiao-Bing  YUAN Guo-Ping  YOU Hui-Chuan  YIN Gong-Ming  TENG Chuan-Kai  XIE Pin  MEI Duo
Institution:1.National field Scientific Observatory Station in Lhasa, Institute of Geology,China Earthquake Administration, Beijing 100029,China;2.Earthquake Prediction Institute, China Earthquake Administration, Beijing 100036,China;3.Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China;4.Geological Institute of Zhejiang Oilfield Company, Hangzhou 310013, China;5.Xizang Earthquake Bureau, Lhasa  850000, China
Abstract:Through studying of magnetotelluric sounding on Qushui-Duodi profile in Lhasa basin, the deep structures of Lhasa basin are reconstructed. Granite is extensively distributed in the upper crust. The depth of Moho surface is about 70 kilometers. There is a high conductivity layer in the crust, the top surface of the layer rises gradually from south to north, and the thickness of the layer is 20~30 kilometers. There exists a deep fault near Sangda area.
Keywords:Lhasa basin  MT exploration  Crust-mantle structure
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