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Method for modeling kinematic seismic data which has undergone processing by at least one displacement operator.

机译:对已经由至少一个位移算子进行处理的运动地震数据进行建模的方法。

摘要

A method for modelling kinematic seismic data processed with at least one motion operator, wherein the mid-point (N1) of a transmitter (S)/receiver (R) system is determined, a ray tracing for the system is established relative to a given reflector, the ray parameters are processed using a motion operator to provide a first arrival point (N'1) located on the model, the position deviation ( DELTA E) between the reference points (N) and the point (N'1) is determined and compared with a predetermined deviation ( DELTA e), and an iteration is performed on each new arrival point (N'i) until the deviation ( DELTA E) is the same as or smaller than the predetermined deviation ( DELTA e). The method is particularly useful in tomography.
机译:一种用至少一个运动算子处理的运动地震数据建模的方法,其中确定发射器(S)/接收器(R)系统的中点(N1),相对于给定给定系统的射线跟踪反射器,使用运动算子处理射线参数以提供位于模型上的第一到达点(N'1),参考点(N)和点(N'1)之间的位置偏差(DELTA E)为确定并与预定偏差(Δe)进行比较,然后对每个新到达点(N'i)进行迭代,直到偏差(DEL E)等于或小于预定偏差(Δe)。该方法在断层摄影中特别有用。

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