结果表明，地电阻率各向异性度(S)异常变化中的地震前兆信息量大于地电阻率异常变化中的地震前兆信息量。
The results show that more information was received from the variation of s than from that of ground resistivity.
由此算出岩石各向异性系数，并对水平井电阻率曲线进行校正。
With these data, an anisotropy factor can be calculated, and the horizontal well log curves can be corrected.
尽管随钻电阻率测井具有诸多优点，但其仍然要受井下测量环境的影响，其主要的环境影响因素是各向异性。
Although logging-while-drilling resistivity logging has many advantages, it is influenced by the down-hole measurement environment, mainly anisotropy.
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