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HYBRID IMAGE OF EARTH FORMATION BASED ON TRANSIENT ELECTROMAGNETC MEASUREMENTS

机译:基于瞬变电磁测量的地球形成混合图像

摘要

A method for imaging an earth formation includes estimating an apparent resistivity (AR) value and an apparent distance to a bedding plane (AD2B) value for each of a plurality of samples derived from measurements of a time-dependent transient electromagnetic signal, estimating an inversion-based resistivity value (IB-R) and an inversion-based distance to a bedding plane (IB-D2B) value at a first sample of each consecutive depth interval, wherein each depth interval includes a plurality of consecutive samples, and determining a difference between apparent values and the corresponding inversion-based values. The method further includes generating an image of the earth formation using the AR and AD2B values for the entire interval if the difference is less than a threshold value and generating an image of the earth formation using IB-R and IB-D2B values for the entire interval if the difference is greater than the threshold value.
机译:一种用于对地球地层成像的方法,包括针对从随时间变化的瞬变电磁信号的测量结果得出的多个样本中的每一个,估计视电阻率(AR)值和与层理面(AD2B)值的表观距离;估计反演连续深度间隔的第一个样本处的基于电阻率的值(IB-R)和距地层的反演距离(IB-D2B),其中每个深度间隔包括多个连续的样本,并确定差在视在值和相应的基于反转的值之间。该方法还包括:如果差小于阈值,则使用整个间隔的AR和AD2B值生成地层图像;以及使用整个间隔的IB-R和IB-D2B值生成地层图像。如果差异大于阈值,则间隔。

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