Simultaneous model-based inversion of pre-stack 3D seismic data targeting a deep geothermal reservoir, Northwest Hungary

IF 1.4 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS Acta Geodaetica et Geophysica Pub Date : 2023-02-16 DOI:10.1007/s40328-023-00404-z
Emad N. Masri, Ernő Takács
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Abstract

The well-known, traditional way to extend P-wave acoustic impedance data between and beyond the well log locations is the post-stack inversion of seismic data usually available in the surroundings of the boreholes. A relatively new trend in the seismic exploration is based on the pre-stack inversion of the seismic CDP gathers providing both the P- and S-wave acoustic impedance sections (and volumes), as well as the estimated density data. This methodology is often called as simultaneous model-based inversion and can be utilized not only for hydrocarbon exploration, but it might also be a useful tool for the investigation of geothermal resources. In this study, we will compare the results of post-stack and pre-stack acoustic impedance inversions utilizing the same seismic volume. We will demonstrate and analyze the inverted attribute sections (and some of their derivatives) obtained by the pre-stack algorithm in detail. Finally, we will draw the conclusions about the lithological discrimination of the studied complex carbonate geothermal reservoir located in the pre-Cenozoic basement of the Little Hungarian Plain.

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基于模型的匈牙利西北部深层地热储层叠前三维地震数据同步反演
众所周知,将纵波声阻抗数据扩展到测井位置之间和之外的传统方法是对通常在井眼周围可用的地震数据进行叠后反演。地震勘探的一个相对新的趋势是基于地震CDP集的叠前反演,提供P波和s波声阻抗剖面(和体积)以及估计密度数据。这种方法通常被称为基于模型的同步反演,不仅可以用于油气勘探,也可以用于地热资源的调查。在这项研究中,我们将比较使用相同地震体积的叠后和叠前声阻抗反演结果。我们将详细演示和分析由堆栈前算法获得的倒属性部分(及其一些衍生部分)。最后,对小匈牙利平原前新生代基底的复杂碳酸盐岩地热储层进行了岩性识别。
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来源期刊
Acta Geodaetica et Geophysica
Acta Geodaetica et Geophysica GEOCHEMISTRY & GEOPHYSICS-
CiteScore
3.10
自引率
7.10%
发文量
26
期刊介绍: The journal publishes original research papers in the field of geodesy and geophysics under headings: aeronomy and space physics, electromagnetic studies, geodesy and gravimetry, geodynamics, geomathematics, rock physics, seismology, solid earth physics, history. Papers dealing with problems of the Carpathian region and its surroundings are preferred. Similarly, papers on topics traditionally covered by Hungarian geodesists and geophysicists (e.g. robust estimations, geoid, EM properties of the Earth’s crust, geomagnetic pulsations and seismological risk) are especially welcome.
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