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Method for determining earth vertical electrical anisotropy in marine electromagnetic surveys

机译:海洋电磁勘测中确定地球垂直电各向异性的方法

摘要

A method is disclosed for determining earth vertical electrical anisotropy from offshore electromagnetic survey measurements. The method requires both online and offline data, which includes at least one electromagnetic field component sensitive at least predominantly to vertical resistivity and another component sensitive at least predominantly to horizontal resistivity. Using a horizontal electric dipole source, online EZ and offline HZ measurements are preferred. For a horizontal magnetic dipole source, online HZ and offline EZ data are preferred. magnetotelluric data may be substituted for controlled source data sensitive to horizontal resistivity. Maxwell's equations are solved by forward modeling or by inversion, using resistivity models of the subsurface that are either isotropic or anisotropic.
机译:公开了一种用于根据离岸电磁勘测测量确定地球垂直电各向异性的方法。该方法需要在线和离线数据,其包括至少一个至少主要对垂直电阻率敏感的电磁场分量和另一个至少主要对水平电阻率敏感的电磁场分量。使用水平电偶极子源时,首选在线E Z 和离线H Z 测量。对于水平磁偶极子源,首选在线H Z 和离线E Z 数据。大地电磁数据可以替代对水平电阻率敏感的受控源数据。通过使用各向同性或各向异性的地下电阻率模型,通过正演建模或通过反演求解麦克斯韦方程。

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