库页岛陆架水域异常地层压力分布特征

A. K. Shatyrov
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引用次数: 0

摘要

介绍。利用钻孔资料分析了库页岛陆架水域异常地层压力分布的条件。分析库页岛陆架异常高孔隙压力带(AHPP)和异常高地层压力带(AHFP)的成因,识别其孔隙压力非均质性。材料和方法。数据系统化和统计概括,部分借鉴实地数据、参考文献和出版资料。利用PetroMod软件(斯伦贝谢)对AHPP (AHFP)地层过程进行建模。研究发现,库页岛陆架的孤立浅海浅沉积带与同生浅海浅沉积带有关,通常出现在由三角洲沉积物组成的区域倾角下发育的相中,随后形成于内浅海(海底含水和近海沉积物)和中浅海(浅海沉积物)环境中,即在质量积累速率较大的地方。从这一位置出发,研究了库页岛陆架古阿穆尔河三角洲沉积物中的ahfp。各种程序和直接井眼测量证明了AHPP (AHFP)层的剖面存在。在库页岛大陆架范围内,几个井眼记录到地层压力的增加,即显示出异常高地层压力区(AHFP)。AHFP的形成过程应基于岩石压实过程的知识,以及岩石的初始、最终和正常孔隙度、密度和压力的知识进行建模。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Distribution characteristics of abnormal formation pressures in the aquatic area of the Sakhalin shelf
Introduction. The conditions determining the distribution of abnormal formation pressures in the aquatic area of the Sakhalin shelf are analysed using boring data.Aim. To analyse the genesis of abnormally high pore pressure (AHPP) or abnormally high formation pressure (AHFP) zones and identify the pore pressure heterogeneities of the Sakhalin shelf.Materials and methods. Data systematization and statistical generalization, partial borrowing of materials from field data, reference literature and published materials. Modelling of the AHPP (AHFP) formation process was performed using the PetroMod software (Schlumberger).Results. The study revealed the isolated AHPP zones of the Sakhalin shelf, related to the syngenetic AHPPs and typically encountered in facies that develop downward the regional dip and consist of deltaic sediments, formed subsequently in the environments of internal neritic (subsaline-aqueous and offshore-marine sediments) and middle neritic (shallow marine sediments) zones, i.e., in places with the large mass accumulation rate. From this position, the AHPPs (AHFPs) in the Paleo-Amur deltaic sediments of the Sakhalin shelf were studied. Various procedures and direct borehole measurements proved the sectional presence of AHPP (AHFP) zones. Within the limits of the Sakhalin shelf, an increase in the formation pressure is recorded in several boreholes, i.e., zones of abnormally high formation pressure (AHFP) are revealed. The process of forming AHPP (AHFP) should be modelled based on the knowledge about the compaction processes of rocks, as well as their initial, final and normal porosity, density and pressure.
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