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Method for obtaining commuting times of reflection from an interpretation of the data su00ecsmicos wavelength cilu00ecndrica migrada

机译:通过对数据s的解释来获得反射的通勤时间的方法

摘要

Method for obtaining commuting times of reflection from an interpretation of the data su00ecsmicos wavelength cilu00ecndrica migrada ".Method for obtaining commuting times of reflection from an interpretation of seismic data in cylindrical waves migrated.For a given value of the parameter defining the slope of these waves, or the superposition of these data associated with multiple rows of substantially parallel acquisition, this parameter.Possibly, taking different values successively.The method comprises the following steps: a) definition of a vector of slowness ( sym ) whose component (PX) in a direction parallel to the lines of the acquisition, defines the slope of the cylindrical wave; (b)For a given position of a seismic receiver of abscissa (x ~ R ~) in a line of purchase, demand of abscissa ( sym ) of the source.So that a ray starting from seismic receiver and reflecting in an event captured from the source on the line acquisition considered,With a vector of slowness ( sym ) whose component in the direction parallel to the lines of the acquisition is (- P ~ x ~); c) determining a travel time (T ^ and ^ (x ~ R ~)) by adding the value of the timeThe displacement along the radius of a time equal to the product of inclination (P ~ x ~) of cylindrical wave by the abscissa of point source; (d) the repetition of stages (b) and (c) for all positions of the receiver andS to which a result of demigrau00e7u00e3o is sought; and (E) the repetition of steps a) to d) for all lines of acquisition for which a result of demigrau00e7u00e3o is wanted, and for all VALaw taken by parameter (P ~ x ~). Applications: analysis of speed of demigrau00e7u00e3o for determining the distribution of speeds of propagation of seismic waves in the subsoil, for example.
机译:通过解释数据s u00smicos波长cil u00ecndrica migrada “获得反射通勤时间的方法。”通过从迁移的圆柱波中地震数据的解释获得通勤时间的方法。对于给定的参数定义这些波的斜率,或与多行基本平行采集相关的数据的叠加,此参数。可能,相继采用不同的值。该方法包括以下步骤:a)定义慢度矢量( )其分量(PX)在平行于采集线的方向上定义了圆柱波的斜率;(b)对于横坐标(x〜R〜)的地震接收器在购买线上的给定位置,考虑到源的横坐标()的需求,因此考虑到线捕获,从地震接收器开始并在从源捕获的事件中反射的光线会考虑在线路采集中, sym>),其在平行于采集线的方向上的分量为(-P〜x〜); c)通过将时间值相加来确定传播时间(T ^和^(x〜R〜))沿时间半径的位移等于圆柱波的倾斜度(P〜x〜)与横坐标的乘积点源(d)重复步骤(b)和(c),以求接收器和S的所有位置,并向其中求出半音的结果; (E)对所有需要demigra u00e7 u00e3o结果的采集行以及参数(P〜x〜)进行的所有VALaw重复步骤a)至d)。应用:例如,通过分析demigra u00e7 u00e3o的速度来确定地层中地震波的传播速度分布。

著录项

  • 公开/公告号BR0106153A

    专利类型

  • 公开/公告日2002-08-13

    原文格式PDF

  • 申请/专利权人 INSTITUT FRANCAIS DU PETROLE;

    申请/专利号BR20010106153

  • 发明设计人 FREDERIC ASSOULINE;PATRICK LAILLY;

    申请日2001-12-19

  • 分类号G01V1/30;

  • 国家 BR

  • 入库时间 2022-08-22 00:46:06

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