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METHOD FOR DETERMINING WAVE FIELD, FREE OF FALSE REFLECTED SIGNALS, EMITTED BY MARINE SEISMIC SOURCE (OPTIONS)

机译:确定海洋地震源发射的无虚假反射波的波场的方法(选件)

摘要

Seismic data is obtained by activating the first seismic source at the first moment of time and one or more seismic sources at their characteristic time points relative to the time of recording signals, while the sources are substantially connected and located at different depths. The first wave field is determined, which would have arisen if the first source had been activated at a point in time selected relative to the start time of the recording, and adjusted in time taking into account the depth of the water. One or more additional wave fields are determined that would have arisen if one or each of several additional sources had been activated at a specified point in time, selected in relation to the specified time for the start of recording, and adjusted in time taking into account the depth of one or more additional sources in water. The first wave field is combined with one or more additional wave fields to determine a wave field with suppressed false reflections, corresponding to the activation of a single seismic source.
机译:地震数据是通过在第一时刻激活第一地震源以及在相对于记录信号的时间的特征时间点激活一个或多个地震源而获得的,而这些震源实际上是相连的并且位于不同的深度。确定第一波场,如果在相对于记录的开始时间选择的时间点激活了第一声源并考虑到水的深度及时调整了第一波场,就会产生第一波场。确定如果在指定的时间点激活了几个其他信号源中的一个或每个信号源,相对于指定时间进行选择以开始记录并在考虑到时间的情况下进行了调整,则会产生一个或多个其他波场。水中一种或多种其他来源的深度。将第一波场与一个或多个其他波场组合,以确定具有抑制的虚假反射的波场,对应于单个地震源的激活。

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