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龙门山逆冲构造带大地电磁测深初步成果

Preliminary result of magnetotelluric sounding in the Longmen thrust belt of West Sichuan,China

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【作者】 王绪本余年朱迎堂徐权辉黄文彬高树全

【Author】 WANG Xu-ben1,2,YU Nian1,3,ZHU Ying-tang1,2,XU Quan-hui1,HUANG Wen-bin1,GAO Shu-quan11.Key Laboratory of Earth Exploration and Information Technology of MOE,Chengdu University of Technology,Chengdu 610059,China;2.College of Information Engineering,Chengdu University of Technology,Chengdu 610059,China;3.China Railway Eryuan Engineering Group Co.Ltd,Chengdu 610031,China

【机构】 成都理工大学"地球探测与信息技术"教育部重点实验室

【摘要】 通过对穿过龙门山逆冲构造带中段松潘-中江大地电磁观测资料的处理和反演解释,揭示了松潘-甘孜褶皱带、龙门山及川西前陆盆地30 km深度的地壳电性结构,发现龙门山-松潘地壳15~20 km深部存在西倾连续的壳内高导层,大地电磁测深结果明显显示龙门山深部逆冲推覆构造特征。龙门山深部电性结构初步研究,对于分析其与相邻构造单元的关系,研究青藏高原东缘陆内造山带深部地球动力学过程都具有重要理论意义。

【Abstract】 By processing,interpreting and inversing the magnetotelluric observation data obtained from Songpan-Zhongjiang passed through the middle section of the Longmen thrust belt,this paper reveals 30 km deep crust architecture of the Songpan-Ganzi fold belt,Longmen Mountains and West Sichuan foreland basin,and finds the west inclined successive high conductive layer in the crust of 15~20 km of Longmen Mountains.The magnetotelluric sounding result evidently demostrates the features of the Longmen thrust belt in the deep.This result is of important theoretical significance for detecting the deep fine structures of Longmen Mountains and revealing its relationship with the adjacent tectonic units and the continental orogenic deep geodynamics process on the eastern edge of the Qinghai-Tibet Plateau.

【基金】 国家自然科学基金资助项目(40674035);国家863高技术研究发展计划项目(2006AA06Z110)
  • 【文献出处】 成都理工大学学报(自然科学版) ,Journal of Chengdu University of Technology(Science & Technology Edition) , 编辑部邮箱 ,2008年04期
  • 【分类号】P631.325
  • 【被引频次】76
  • 【下载频次】704
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