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FREQUENCY-BASED HORIZON INTERPRETATION BASED ON SEISMIC DATA

机译:基于地震数据的基于频率的水平解释

摘要

Seismic data obtained from a seismic survey conducted of a subterranean region is received. The seismic data includes multiple frequency components, having a frequency bandwidth. A target, to-be-picked horizon is identified by displaying well data on the seismic section and correlating the seismic reflector with layer tops in the well data. A horizon represents a seismic reflector between two geological layers in the subterranean region. A single frequency that gives rise to a predetermined continuity along the target horizon is determined from the frequency bandwidth of the seismic data. The seismic data is filtered to mono-frequency volumes. The mono-frequency seismic volumes include a single frequency component. A horizon is picked corresponding to the target horizon based on the mono-frequency volumes. The identified horizon corresponding to the target horizon is output for determining geological features of the subterranean region based on the identified horizon.
机译:接收从地下区域进行的地震勘测获得的地震数据。地震数据包括具有频率带宽的多个频率分量。通过在地震剖面上显示油井数据并将地震反射器与油井数据中的层顶相关联,可以确定待采的目标层。地平线表示地下区域中两个地质层之间的地震反射器。从地震数据的频率带宽确定沿目标水平线产生预定连续性的单个频率。地震数据被过滤为单频体积。单频地震体包括一个单频分量。基于单频量选择与目标地平线相对应的地平线。输出与目标地平线相对应的识别出的地平线,用于基于识别出的地平线来确定地下区域的地质特征。

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