日本山川地热田多模态地球物理资料三维反演与解释

M. Endo, M. Zhdanov, A. Gribenko, D. Sunwall, Takuya Miura, Hisako Mochinaga, N. Aoki, T. Mouri
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引用次数: 1

摘要

地热田的勘探和开发需要对不同的地球物理资料进行定量解释。本文介绍了多模态地球物理数据三维反演和解释的新方法,该方法结合了已知的地质/地球物理约束条件。一般情况下,地球物理逆问题是不适定的,即它是非唯一的和不稳定的;然而,适当的先验信息可以帮助减少非唯一性,提高该病态问题的稳定性。开发的方法使用由已知信息“引导”的反演原理。在该方法的框架中,三维反演本身是数据驱动的,但在迭代反演过程中使用先验的地质/地球物理模型作为初始和参考模型。本文将该方法应用于日本山川地热田的大地电磁、重磁资料综合解释,利用同一地区地震和测井资料的约束条件。结果表明,该方法可生成可靠的不同物性的三维模型,为研究区复杂地下构造的地质解释提供了坚实的基础,对地热勘探具有重要意义。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Three-Dimensional Inversion and Interpretation of Multimodal Geophysical Data in Yamagawa Geothermal Field, Japan
Summary Exploration and development of geothermal fields requires quantitative interpretation of different geophysical data. In this paper, we introduce the novel approach to three-dimensional inversion and interpretation of multimodal geophysical data, which incorporates the known geological/geophysical constraints. In a general case, geophysical inverse problem is ill-posed, i.e., it is non-unique and unstable; however, appropriate a priori information can help reducing the nonuniqueness and increasing the stability of this ill-posed problem. The developed approach uses the principles of inversion “guided” by known information. In the framework of this approach, the 3D inversion itself is data driven, but a priori geological/geophysical model is used as the initial and reference model during the iterative inversion process. We have applied the developed method to the integrated interpretation of magnetotelluric, gravity, and magnetic data in Yamagawa geothermal field of Japan, using the constraints based on seismic and well-logging data acquired in the same area. The results have demonstrated that the developed method produces reliable 3D models of different physical properties, which provide a solid basis for geological interpretation of the complex subsurface structures in the survey area, critical for geothermal exploration.
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