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川西—藏东大地电磁资料的阻抗张量畸变分解

IMPEDANCE TENSOR DISTORTION DECOMPOSITION OF MAGNETOTELLURIC DATA FROM WEST SICHUAN-EAST XIZANG

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【作者】 晋光文孙洁白登海王立凤

【Author】 JIN GUANGWEN SUN JIE BAI DENGHAI WANG LIFENG Institute of Geology,China Scismological Bureau,Beijing 100029,China

【机构】 中国地震局地质研究所

【摘要】 根据Swift和Bahr的分解结果,得到准三维/二维模型的区域构造和各个畸变因子,应用于川西—藏东MT剖面资料的分析,结果表明:该地区的构造特点为浅部比较简单,深部相对复杂;以雅安为界,东部构造比西部构造简单,而且比较稳定;构造主轴方位基本在近南北向,其偏差很少超过30°;分解参效对几条大的断裂有较好的显示;测线1横穿3个主要构造单元,并被几条大断裂切割,构造最复杂;测线2接近3D/2D模型;测线3具有较强的静位移畸变.

【Abstract】 We have obtained the regional structure of a quasi-3D/2D model and distortion factors from the result of Swift and Bahr’s decomposition in analysis of magnetotelluric data of West Sichuan-East xizang sounding profiles.The result shows that the structure of the region along these profiles is simple in the shallow part and relatively complex in the deep part.Taking the Ya’ an line as a boundary,we find that the structure in the eastern part is simpler and more stable than that in the western part.The orientation of major structural axis is basically in nearly S-N direction and its deviations are Seldom more than 30°.The decomposed parameters can well express several major faults.The first sounding line runs across 3 major tectonic units and several major faults,so the structure is most complex.The second sounding line is close to a 3D/2D model,and the third sounding line exhibits stronger static displacement distortion.

【基金】 国家重点基础研究发展规划“973”项目(G9513-02-03)
  • 【会议录名称】 中国科学院地质与地球物理研究所二○○三学术论文汇编·第二卷(青藏高原)
  • 【会议名称】中国科学院地质与地球物理研究所2003学术年会
  • 【会议时间】2003-12-01
  • 【会议地点】中国北京
  • 【分类号】P631.325
  • 【主办单位】中国科学院地质与地球物理研究所(Institute of Geology and Geophysics Chinese Academy of Sciences)
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