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METHOD OF PRODUCING MIGRATED SEISMIC IMAGES OF GEOLOGIC MEDIA BASED ON 2D SEISMIC SURVEY DATA

机译:基于二维地震勘测数据的地震介质移动影像成像方法

摘要

FIELD: physics.SUBSTANCE: invention relates to geophysics and can be used to produce migrated seismic images of geologic media from 2D seismic survey data in the form of an amplitude depth or time section for geological prospecting. Essence of the proposed method consists in the fact that each amplitude of seismic traces of all seismograms of common points of excitation (OTP) on the basis of knowledge of effective velocities and inclination angles of reflecting boundaries are carried in section into points of their origin, and then to the nearest centre of cells (bin) previously formed in a vertical plane passing through the observation profile, networks of selected dimensions along the vertical and horizontal. After transformation of all traces obtained for other positions of excitation and reception points on the profile, accumulation of all amplitudes is performed in bin centres. This makes it possible to obtain total amplitudes A(x,z) in the nodes of the created network, which characterize actual reflecting capacity of the medium. Accumulated amplitudes make it possible to form a seismic image of the geologic environment in a form familiar to seismic prospecting.EFFECT: technical result is high information value of obtained data by obtaining real migrated seismic images of medium.1 cl, 1 dwg
机译:技术领域本发明涉及地球物理学,并且可以用于从二维地震勘测数据以振幅深度或时间段的形式产生地质介质的迁移的地震图像,以用于地质勘探。所提方法的实质在于,在有效速度和反射边界的倾角知识的基础上,将所有公共激发点(OTP)地震图的地震迹线的每个振幅都切入其原点,然后再到达先前在通过观察轮廓的垂直平面中形成的单元(仓)的最近中心,即沿垂直和水平方向具有选定尺寸的网络。在对轮廓上的激发点和接收点的其他位置获得的所有迹线进行转换后,将在仓位中心进行所有振幅的累加。这使得有可能在所创建的网络的节点中获得总振幅A(x,z),该总振幅表征了介质的实际反射能力。累积的振幅使得有可能以地震勘探熟悉的形式形成地质环境的地震图像。效果:技术结果是通过获取介质的真实偏移地震图像获得的数据具有很高的信息价值。1cl,1 dwg

著录项

  • 公开/公告号RU2018105637A3

    专利类型

  • 公开/公告日2019-08-14

    原文格式PDF

  • 申请/专利权人

    申请/专利号RU20180105637

  • 发明设计人

    申请日0000-00-00

  • 分类号G01V1/28;

  • 国家 RU

  • 入库时间 2022-08-21 11:46:48

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