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首页> 外文期刊>Energy sources. Part A, Recovery, utilization, and environmental effects >Compaction of Clays as a Factor in the Formation of Hydrodynamic Regime and Hydrocarbon Migration and Accumulation
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Compaction of Clays as a Factor in the Formation of Hydrodynamic Regime and Hydrocarbon Migration and Accumulation

机译:粘土压实是形成水动力区和油气运移与聚集的一个因素

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摘要

Based on extensive experience, the writers present relationships (1) between the porosity and depth of burial, and (2) between the permeability and depth of burial in undercompacted thick argillaceous sequences. They also explain the formation of abnormally high formation pressures (AHFP) and mode of oil/gas migration and accumulation. Special emphasis is placed on petroliferous deposits of Azerbaijan.
机译:基于丰富的经验,作者提出了(1)孔隙度与埋藏深度之间的关系,以及(2)在压实较厚的泥质层序中埋藏的渗透率与埋藏深度之间的关系。他们还解释了异常高的地层压力(AHFP)的形成以及油气运移和聚集的模式。特别强调的是阿塞拜疆的含油矿床。

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