裂缝致TTI介质中pp波方位反射系数研究

IF 2.1 4区 地球科学
Han Xiao, Xinmin Shang, Guoqiang Shen
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引用次数: 0

摘要

页岩裂缝是页岩油气勘探开发的重要研究对象之一。在地震剖面中,分辨率被认为是地震本征波长的四分之一。长度小于分辨率的裂缝通常表现为地震走时和振幅的方位各向异性。介质中包含一组倾斜裂缝,可以近似为TTI介质。对于倾斜裂缝诱发的TTI介质,提出了基于线性滑移理论和各向异性参数的处理方法,根据背景介质和裂缝的特征计算方位反射系数。为了验证该过程的准确性,我们设计了数值试验,并在此基础上研究了裂缝极角和裂缝密度对诱导TTI介质AVAZ特性的影响。与现有方法相比,该方法不需要介质的各向异性对称性和取向等先验信息,可以根据背景介质和裂缝的特征直接计算裂缝诱导介质的方位反射系数。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Study of PP-wave azimuthal reflection coefficients in fracture-induced TTI media

The fracture in shale is one of the most important research objectives of shale oil and gas reservoirs’ exploration and development. In seismic profiles, the resolution is considered as one-fourth of the seismic eigen wavelength. Fractures whose length are less than the resolution are usually shown as the azimuthal anisotropy of seismic travel times and amplitude. Media contain one set of tilted fractures that could be approximated as TTI media. For TTI media induced by tilted fractures, we proposed a process based on linear slip theory and anisotropic parameters, in which we could calculate azimuthal reflection coefficients by the characteristics of background media and fractures. We designed numerical tests to verify the accuracy of the process, and based on the process, we studied the influence of the polar angles and densities of fractures on the AVAZ characteristics of the induced TTI media. Compared with present methods, the proposed method could be conducted without the prior information about the anisotropy symmetry and orientation of the media and could directly calculate the azimuthal reflection coefficient of the fracture-induced media according to the characteristics of background media and fractures.

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来源期刊
Acta Geophysica
Acta Geophysica GEOCHEMISTRY & GEOPHYSICS-
CiteScore
3.80
自引率
13.00%
发文量
251
期刊介绍: Acta Geophysica is open to all kinds of manuscripts including research and review articles, short communications, comments to published papers, letters to the Editor as well as book reviews. Some of the issues are fully devoted to particular topics; we do encourage proposals for such topical issues. We accept submissions from scientists world-wide, offering high scientific and editorial standard and comprehensive treatment of the discussed topics.
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