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System for the Attenuation of Water Bottom Multiples in Seismic Data Recorded by Pressure Sensors and Particle Motion Sensors

机译:压力传感器和质点运动传感器记录的地震数据中水底多重波衰减系统

摘要

An up-going wavefield and a down-going wavefield are calculated at a sensor position from a pressure sensor signal and a particle motion sensor signal. Then, an up-going wavefield is calculated at a water bottom position substantially without water bottom multiples from the up-going and down-going wavefields at the sensor position. In one embodiment, the up-going wavefield at the sensor position is backward propagated to the water bottom, resulting in an up-going wavefield at the water bottom. The down-going wavefield at the sensor position is forward propagated to the water bottom, resulting in a down-going wavefield at the water bottom. The up-going wavefield at the water bottom without water bottom multiples is calculated from the backward propagated up-going wavefield at the water bottom, the forward propagated down-going wavefield at the water bottom, and a reflection coefficient of the water bottom.
机译:根据压力传感器信号和粒子运动传感器信号在传感器位置计算上行波场和下行波场。然后,从传感器位置处的向上和向下波场中,在基本没有水底倍数的情况下,在水底位置处计算向上波场。在一实施例中,传感器位置处的上行波场向后传播到水底,从而在水底处产生上行波场。传感器位置的下行波场被向前传播到水底,导致水底的下行波场。根据水底的后向传播波场,水底的前向传播波场和水底的反射系数,算出没有水底倍数的水底的上行波场。

著录项

  • 公开/公告号GB2430748B

    专利类型

  • 公开/公告日2008-01-23

    原文格式PDF

  • 申请/专利权人 PGS AMERICAS INC.;

    申请/专利号GB20070001911

  • 发明设计人 CLAES NICHOLAI BORRESEN;

    申请日2005-08-23

  • 分类号G01V1/36;G01V1/38;

  • 国家 GB

  • 入库时间 2022-08-21 19:46:34

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