摘要
用EH-4仪器进行音频大地电磁测量,目前已取得了广泛的应用。然而,进行资料的二维反演时,遇到了在大地电磁测深中同样的问题:TE极化模式和TM极化模式不容易辨别。文章介绍了3种有效视电阻率,研究表明,利用有效视电阻率进行二维反演能准确真实的反映地下的介质模型。经实际资料处理证明,此方法效果明显。
Continuous conductivity imaging system of EH -4 for magnetotelluric sounding is used widely. However, two-dimensional inversion of EH-4 data has a problem. It is difficult to make distinguish TE and TM mode which is existed in magnetotelluric sounding. Three effective apparent resistivities are introduced. It is shown that that effective apparent resistivity for two - dimensional inversion can really reflect geo - electric model, and can remove static shift. This method is proved effectively during data processing in practice.
出处
《地质与勘探》
CAS
CSCD
北大核心
2008年第3期56-59,共4页
Geology and Exploration
基金
国家自然科学基金项目(编号:60672042)资助
关键词
EH-4系统
大地电磁测深
有效视电阻率
二维反演
EH-4 system, magnetotelluric sounding, effective apparent resistivity, two- dimensional inversion