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大地电磁测深资料解释的新方法
A NEW APPROACH FOR INTERPRATATION OF MAGNETOTELLURIC DATA
【摘要】 大地电磁测深 (MT)资料解释中 ,长期以来使用观测的视电阻率作为解释参数。但视电阻率存在一定的局限性。相位微分为MT的解释增加了一种新的手段。从理论上研究了相位微分的性质 ,并将其应用于松辽盆地北部MT资料解释中 ,得出了A剖面的电性特征 ,确定了主要电性层的深度和电阻率。
【Abstract】 In magnetotelluric(MT) data analysis, the observed apparent resistivity have been used as an interpretative parameter for a long time. However, apparent resistivity has limitations. There is new approach for interpratation of magnetotelluric data by using the method of phase-derivative. In this paper the specific property of phase-derivative was studied and used in the interpretation of MT data from northern Songliao basin. Electric features of profile A were thus obtained. The depth and resistivity of primary electric layers were delimited.
【关键词】 电阻率;
阻抗相位;
相位微分;
解释参数;
【Key words】 resistivity; impedance phase; phase-derivative; interpretative parameter;
【Key words】 resistivity; impedance phase; phase-derivative; interpretative parameter;
【基金】 国家自然科学基金委员会资助;大庆石油管理局资助项目!(49894190 - 31)
- 【文献出处】 长春科技大学学报 ,JOURNAL OF CHANGCHUN UNIVERSITY OF SCIENCE AND TECHNOLOGY , 编辑部邮箱 ,2000年03期
- 【分类号】P631.325
- 【被引频次】17
- 【下载频次】253