Features of high-density transient electromagnetic sounding data inversion under oil and gas prospecting in the Nepa-Botuoba anteclise area

E. Murzina, A. Pospeev, I. Seminskiy, I. Buddo, D. B. Nemtseva, V. S. Emelianov, Y. Agafonov
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引用次数: 2

Abstract

The data of near-field transient electromagnetic sounding, which are widely used for the purposes of oil and gas exploration within the Nepa-Botuoba anteclise, are typically interpreted in terms of quasi-horizontally-layered models of media. The purpose of this study is to develop an approach to the inversion of transient electromagnetic sounding curves obtained via high-density 3D observation networks. The study was based on mathematical modeling, whose results allowed to estimate the lateral spatial parameters of a non-stationary electromagnetic field as well as to understand the differences between the results of one-dimensional inversion of the transient electromagnetic sounding data and the true parameters of the target horizon. As a result, the characteristic of the electromagnetic field described by an exponential function and used in the lateral-constraint inversion of high-density electromagnetic sounding was obtained. The proposed approach was tested on the practical data within the site under investigation located on the slope of the Nepa-Botuobа anteclise. It is shown that the use of spatial discrepancy under TEM sounding data inversion makes it possible to obtain geoelectric models characterized by lateral consistency of section geoelectric parameters. The application of the spatial stacking-based approach in the inversion process allows to increase the solution stability of the inverse problem of the near-field TEM sounding data.
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nepa—botuoba前陆区高密度瞬变电磁测深资料反演特征
近场瞬变电磁测深数据被广泛用于Nepa-Botuoba板块的油气勘探,通常采用准水平层状介质模型进行解释。本研究的目的是建立一种高密度三维观测网获得的瞬变电磁测深曲线反演方法。该研究基于数学建模,其结果可以估算非平稳电磁场的横向空间参数,并了解瞬变电磁测深数据一维反演结果与目标层位真实参数的差异。得到了用指数函数描述的电磁场特征,并将其用于高密度电磁测深横向约束反演。提议的方法在位于nepa - botuobet anteclise斜坡上的调查场地内的实际数据上进行了测试。结果表明,利用瞬变电磁法测深资料反演的空间差异,可以得到剖面地电参数横向一致的地电模型。在反演过程中应用基于空间叠加的方法,可以提高近场瞬变电磁法探测数据反演问题的求解稳定性。
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