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Integrated gravity-magnetic-electric-seismic inversion

机译:重力-电磁-地震综合反演

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摘要

On the basis of detailed separation gravity field source from magnetic one and comprehensive study of electric field and seismic velocity field, internal relation between various geophysical fields is analyzed quantitatively with the subjective geologic model interpreted by seismic (electric method) data as restraints. By plane iterative inversion, geologic model consists with different kinds of geophysical data is in-versed and simulated. The prominent feature of this method is that it breaks through intensively used gravity-magnetic-electric-seismic combined profile inversion mode (e. g. , LCT software), realizes combined statistical inversion of gravity-magnetic-electric-seismic based on detailed interface separation and recognition of gravity, magnetic field sources and seismic (or electric method) geologic modeling in depth domain.
机译:在详细分离磁源重力场的基础上,对电场和地震速度场进行了综合研究,以主观地质模型为基础,以地震(电法)数据为约束条件,定量分析了各种地球物理场之间的内在联系。通过平面迭代反演,对包含不同种类地球物理数据的地质模型进行反演和模拟。该方法的突出特点是突破了密集使用的重力-电磁-地震联合剖面反演模式(如LCT软件),在详细的界面分离和识别基础上实现了重力-电磁-地震联合统计反演。深度域中的重力,磁场源和地震(或电方法)地质建模。

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