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Method of seismic surveying for resolving the effects of formation anisotropy in shear wave reflection seismic data

机译:解决剪切波反射地震数据中地层各向异性影响的地震勘探方法

摘要

A novel method of seismic exploration has been developed to resolve confusing and distorted shear wave reflection seismic data which can be obtained in areas having anisotropic formations. In particular, the present method of shear wave seismic exploration comprises imparting first shear wave seismic energy into the earth at selected points with a first source having a first polarization with respect to the line of survey, and recording first signals representative of the earth's response with first geophones having a first polarization with respect to the line of survey. Also, second shear wave energy is imparted into the earth at selected points along the line of survey, with a second shear wave source having a second polarization with respect to the line of survey, and recording second signals representative of the earth's response with second geophones having a second polarization with respect to the line of survey. With a measure of the angle between the survey line and a principal axis of an underlying azimuthally anisotropic formation, the first and second signals are inverted to obtain principal component signals in whcih the confusing and distorted shear wave reflection seismic data resulting from anisotropic formations can be ameliorated.
机译:已经开发出一种新颖的地震勘探方法,以解决可在具有各向异性地层的区域中获得的混乱和扭曲的剪切波反射地震数据。特别地,本发明的剪切波地震勘探的方法包括:将第一剪切波地震能量在选定点处施加到地球上,该第一剪切波地震能量具有相对于勘测线具有第一极化的第一源,并记录代表地球响应的第一信号。相对于勘测线具有第一极化的第一地震检波器。而且,第二剪切波能量在沿测量线的选定点处被赋予地球,第二剪切波源相对于测量线具有第二极化,并用第二地震检波器记录代表地球响应的第二信号相对于测量线有第二个极化。通过测量测量线与下层方位各向异性地层的主轴线之间的夹角,可以将第一和第二信号反转,以获得主成分信号,从而可以使由各向异性地层引起的混乱和扭曲的剪切波反射地震数据成为可能。改善了。

著录项

  • 公开/公告号US4933913A

    专利类型

  • 公开/公告日1990-06-12

    原文格式PDF

  • 申请/专利权人 AMOCO CORPORATION;

    申请/专利号US19880226355

  • 发明设计人 LEON A. THOMSEN;

    申请日1988-07-29

  • 分类号G01V1/00;

  • 国家 US

  • 入库时间 2022-08-22 06:07:20

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