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METHOD AND APPARATUS OF ELECTRICAL RESISTIVITY MEASUREMENTS IN GEOLOGICAL FORMATIONS EMPLOYING MODELING DATA

机译:地层构造建模数据中电阻率测量的方法和装置

摘要

A method, and a system, using computer software to measure characteristics of a geologic formation (22) using vertical side scan resistivity measurements (Rm) to model characteristics such as hydrocarbon reservoirs. The method employs modeling data (23) to remove unwanted information from a signal carrying infromation from a signal carrying information concerning the geologic information (11) and models the resistivity of geologic formations. The spatial distribution and orientation to the magnetic fields are the same, differing only by a constant related to the casing attenuation factor (24). The magnetic field outside of the cased borehole is reduced in amplitude by an attenuation factor associated with the liner. The magnetic field produced at a point outside of the liner is a function of the product of term for the attenuation factor of the liner, ke and a term for the response of the geologic formation, f. Both terms are independent of the other. by factoring (28) and removing information concerning the 20th attenuation factor, ke, accurate measurements of the geologic formation may be determined.
机译:一种使用计算机软件来测量地质构造(22)特征的方法和系统,该方法和系统使用垂直侧扫描电阻率测量值(Rm)来对诸如烃类储层的特征进行建模。该方法使用建模数据(23)以从携带有关于地质信息(11)的信息的信号中移除携带信息的信号中的不想要的信息,并且对地质岩层的电阻率进行建模。磁场的空间分布和方向相同,只是与套管衰减系数(24)有关的常数不同。套管井外部的磁场在振幅上降低了与衬管相关的衰减系数。在衬管外部的点处产生的磁场是衬管的衰减因子的项ke与地质构造的响应项f的乘积的函数。这两个术语彼此独立。通过分解(28)并去除有关第20个衰减因子ke的信息,可以确定地质构造的精确测量。

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