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Method for Determining Resistivity Anistropy From Earth Electromagnetic Transient Step Response and Electromagnetic Transient Peak Impulse Response

机译:从地球电磁瞬态阶跃响应和电磁瞬态峰值脉冲响应确定电阻率各向异性的方法

摘要

A method for determining resistivity anisotropy of subsurface rock formations includes imparting a transient electromagnetic field into the subsurface rock formations. Electromagnetic response of the formations is measured at a plurality of offsets from a position of the imparting. For each offset, an arrival time from the imparting is determined of a peak of an impulse response such that the response is related to subsurface horizontal and vertical resistivities. For each offset, a step response of the formations is determined at a time from the imparting selected such that the step response is related substantially only to mean resistivity. The arrival time of the peak of the impulse response and the late time value of the step response are used to determine the resistivity anisotropy.
机译:确定地下岩层的电阻率各向异性的方法包括将瞬变电磁场赋予地下岩层。在距施加位置的多个偏移处测量地层的电磁响应。对于每个偏移,从施加的到达时间确定脉冲响应的峰值,使得该响应与地下水平和垂直电阻率有关。对于每个偏移,从所选择的赋予中一次确定地层的阶跃响应,使得阶跃响应基本上仅与平均电阻率有关。脉冲响应峰值的到达时间和阶跃响应的延迟时间值用于确定电阻率各向异性。

著录项

  • 公开/公告号EP2275838A3

    专利类型

  • 公开/公告日2012-02-22

    原文格式PDF

  • 申请/专利权人 PGS GEOPHYSICAL AS;

    申请/专利号EP20100169699

  • 发明设计人 HOBBS BRUCE ALAN;WERTHMÜLLER DIETER;

    申请日2010-07-15

  • 分类号G01V3/12;

  • 国家 EP

  • 入库时间 2022-08-21 17:15:33

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