基于瞬变电磁法资料的地质剖面弹速性恢复潜力的岩石物性确证

I. Shelokhov, A. Pospeev, I. Buddo
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摘要

俄罗斯东西伯利亚和西西伯利亚地质剖面是一个非常复杂的地震勘探对象。本文研究的目的是研究电阻率与纵波速度之间的岩石物理关系,为利用瞬变电磁法测深预测上段速度模型提供依据。通过对岩石物理函数进行数值模拟,计算了电阻率随纵波速度的变化曲线。数学建模和现场实验结果证明了该方法的有效性,提高了地质模型构建的精度,提高了预测的可靠性。在此基础上,得出了有利于剖面地电特征向速度特征稳定过渡的地质条件。结果表明,该技术能够可靠地重建上段的速度模型。根据所调查问题的性质,使用所开发的方法可以提高地震数据处理的质量,并以最低的成本提高地质剖面边界测绘的准确性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Petrophysical substantiation of geological section elastic-velocity property recovery potential based on TEM data
The geological section of Eastern and Western Siberia (Russia) is a very complicated object for seismic exploration. The research presented in the article is aimed at studying a petrophysical relation between electrical resistivity and P-wave velocity, as a basis for predicting the velocity model of the upper part of the section based on TEM sounding. Having performed a numerical modeling of petrophysical function, the authors calculated the dependency curves of electrical resistivity on the P-wave velocity. The obtained results of mathematical modeling and field experiments have proved the effectiveness of the proposed methodology as it increases the accuracy of geological model construction and enhances prediction reliability. Based on the dependences obtained, conclusions were drawn about the geological conditions favorable for a steady transition of section geoelectric characteristics to the velocity ones. The proposed technology is shown to provide a reliable reconstruction of the velocity model of the upper part of the section. The use of the developed methodology allows to improve the quality of seismic data processing and increase the accuracy of geological section boundary mapping at minimum cost based on the nature of the problem under investigation.
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