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Seismic trace analysis method utilizing a statistical calibration technique for deducing geologic properties

机译:利用统计定标技术推导地震痕迹的地质特征

摘要

The method applies to an underground formation concerning which one has geologic data obtained by coring or logging in wells (W.sub. 1 -W.sub. k) crossing the formation and seismic data which have been obtained by means of a reflection survey of the 3D type. It is based on a statistical calibration technique with a statistical relationship obtained by bringing together the local geologic data (measured in wells) and seismic attributes read on seismic traces (RW.sub.1 -RW.sub.k) obtained in the immediate neighborhood of each well. This calibration allows an empirical relation to be obtained and applied to all the seismic traces of the field in order to infer the associated geologic characteristics therefrom, by taking advantage of the much denser spatial coverage allowed by seismic prospecting.
机译:该方法适用于具有通过对穿过该地层的井(W.sub.1-W.k。)进行取心或测井而获得的地质数据的地下地层,以及通过反射勘测获得的地震数据。 3D类型。它基于一种统计校准技术,具有统计关系,该统计关系通过将本地地质数据(在井中测量)和在附近邻域获得的地震迹线(RW.sub.1-RW.k)上读取的地震属性汇总在一起而获得每口井。通过利用地震勘探所允许的更密集的空间覆盖范围,该校准允许获得经验关系并将其应用于油田的所有地震道,以便从中推断出相关的地质特征。

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