吐哈盆地台北凹陷中下侏罗统致密砂岩储层特征及影响因素

X. Si, Yang Xu, Xin Wang, Huajun Guo, Yazhe Li, X. Shan
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引用次数: 0

摘要

砂岩根据渗透率和孔隙度可分为多种类型。一些学者和研究人员建立了用孔隙度和渗透率对致密砂岩进行分类的标准。渗透率小于1mD,孔隙度小于10%的砂岩可称为致密砂岩。致密砂岩气的勘探开发已成为中国油气勘探的热点(戴杰等,2002)。近年来,吐哈盆地台北凹陷中下侏罗统发现了不同规模的致密砂岩气藏。分析了中下侏罗统致密砂岩的结构和组成,探讨了成岩作用类型,揭示了成岩作用对储层质量的影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Characteristics and Influence Factors of the Middle-Lower Jurassic Tight Sandstone Reservoirs in the Taibei Sag, Turpan-Hami Basin
Sandstone can be divided into many types with reference to permeability and porosity. Some scholars and researchers have established criteria to classify tight sandstone by using porosity and permeability. Sandstone with permeability less than 1mD and porosity less than 10% could be called tight sandstone. Exploration and development of tight sandstone gas has become a hot spot of oil and gas exploration (Dai J. et al., 2002) in China. Quite recently, tight sandstone gas reservoirs of different scales have been discovered in the middle-lower Jurassic of Taibei Sag in Turpan-Hami Basin. The purposes of this paperare to analyze the texture and composition of the middle-lower Jurassic tight sandstones, investigate diagenesis type and reveal the influence of diagenesis on reservoir quality.
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