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Estimating Formation Pore Pressure in Tectonic Compression Zones

机译:估算构造压缩带的地层孔隙压力

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Accurate knowledge of formation pore pressure is a key requirement for safe and cost-effective drilling in overpressured formations. Tectonic compression is an important type of overpressure mechanism, in addition to undercompaction and fluid expansion. However, there is not a valid approach for overpressure estimation in tectonic compression zones. Actually, two lateral stresses are too large to be ignored in tectonic environments. As a consequence, the conventional overpressure estimation methods are not accurate enough for tectonic compression mechanism. This article presents a new approach called the root mean square (RMS) principal stress method that modifies the estimation of pore pressure for tectonic compression zones. The RMS method better considers the characteristics of a 3D stress state. It has been tested in the Kuqa thrust belt of Tarim oilfield where significant tectonic compression commonly exists. Pore pressure estimation of this region shows that the RMS method provides more precise pore pressure estimates than conventional methods.
机译:准确了解地层孔隙压力是在超压地层中安全且具成本效益的钻井的关键要求。除了欠压实和流体膨胀外,构造压缩是一种重要的超压机制。但是,没有一种有效的方法来估算构造压缩带中的超压。实际上,两个横向应力太大,在构造环境中不能忽略。结果,传统的超压估计方法对于构造压缩机制不够精确。本文提出了一种称为均方根(RMS)主应力方法的新方法,该方法修改了构造压缩带孔隙压力的估计。 RMS方法可以更好地考虑3D应力状态的特征。它已经在塔里木油田的库车逆冲带进行了测试,那里通常存在明显的构造压缩作用。该区域的孔隙压力估算表明,RMS方法比常规方法提供了更精确的孔隙压力估算。

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