歧口凹陷中浅层泥岩蚀变校正方法
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摘要
歧口凹陷滨海海域的钻井液大部分采用水基泥浆。由于中浅层地层受钻井液浸泡的影响,泥岩发生蚀变,导致声波时差测井不能反映原状地层的速度信息,从而影响合成记录标定和井约束反演的效果。统计结果表明,随着水基泥浆对地层浸泡的时间增大,泥岩声波时差变大,速度降低。为此必需对泥岩蚀变进行校正,其校正思路是:在划分出砂泥岩剖面后,以受钻井泥浆浸泡时间较短的井作为标准井,按均值方差法将发生泥岩蚀变的井校正到标准井的分布范围内。泥岩蚀变校正结果表明,利用校正后的声波曲线所做合成记录与井旁实际地震记录对应关系更好,而且薄砂层的反演效果也得到了改善。
Water base mud in Qikou depression invades shales in the shallow formation,which leads to shale alteration and errors in acoustic logs that cannot reflect velocities of origin formations.So synthetic seismogram calibration and well-constrain inversion cannot be accurate.Statistics show that shale velocity decreases with the soak time.After dividing the sand and shale profile,mean and variance methods can be used to calibrate shale alteration basing on short time soak well as a reference.Applications reveal that synthetic seismogram calibration and reservoir inversion of thin sands are better with shale alteration corrected acoustic log.
引文
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