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APPLICATION OF SEISMIC SEDIMENTOLOGY IN ANALYSIS ON CHANNEL SEDIMENTARY FACIES

机译:地震沉积学在通道沉积相分析中的应用

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In this paper, based on the theory of seismic sedimentology, isochronal reference layer is selected in sdmiddle sub-member of H area, to establish proper strata slices, and pick up the seismic attributes of various strata slices. Based on fine calibration between sandstone in wells and plane seismic attributes, multiple attributes of plane strata slices are analyzed to gain the distribution map of sedimentary facies in plane. The distribution of sedimentary facies is proven by the subsequent drilling wells, which proves that seismic sedimentology is a powerful tool to study sedimentary facies and predict favorable accumulation targets when applicable.
机译:本文基于地震沉积物理论,在H区域的Sdmiddle子构件中选择等时参考层,建立适当的地层切片,并拾取各种层面切片的地震属性。基于井和平面地震属性的砂岩之间的细校准,分析了平面层切片的多个属性,以获得平面沉积相的分布图。随后的钻井井被证明,沉积相的分布证明了地震沉积物是研究沉积相的强大工具,并在适用时预测有利的积累目标。

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