库车凹陷迪北地区阿河地层致密储层物性下限及分类评价标准

IF 1.7 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY
Caiyuan Dong, Wei Yang, Jun Li, Dejiang Li, Xueqiong Wu, Weidong Miao, Haihua Zhu, Xilin Yang
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引用次数: 0

摘要

地北地区阿河地层是北部构造带天然气勘探的重点地层。根据地层测试、物性等地质资料,采用经验统计法、分布函数法、含油发生法、约束流体饱和度法等方法合理确定致密储层。并进一步分析了不同方法的含油物性下限。利用高压汞侵入数据对致密砂岩的孔喉结构进行了表征,并结合分形理论和物性数据建立了地北地区阿河地层致密砂岩的分类评价标准。结果表明,地北地区阿河地层致密储层物理极限孔隙度下限为 2.4%,渗透率下限为 0.021×10-3 μm2。根据注汞曲线的分形维数特征,可划分出四类孔隙(裂缝、大孔、中孔、小孔)的不同结构特征,边界值分别为 3000、1000、100 nm;可将地北地区阿河地层致密储层划分为四类:(a)Ⅰ型储层(Ф >7%),主要由断裂和大孔隙组成;(b)Ⅱ型储层(4% <Ф <7%),主要由大孔隙和中孔隙组成;(c)Ⅲ型储层(2% <Ф <4%),主要由中孔隙形成;(d)Ⅳ型储层(Ф <2%),以小孔隙为主,中孔隙次之。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Lower limits of physical properties and classification evaluation criteria of the tight reservoir in the Ahe Formation in the Dibei Area of the Kuqa depression
The Ahe Formation in the Dibei Area is a key natural gas exploration formation in the northern structural belt. Based on geological data such as formation tests and physical properties, the tight reservoirs were determined using the empirical statistics method, distribution function method, oil-bearing occurrence method, and bound fluid saturation method reasonably. The lower limit of the oil-bearing physical properties of the layer was further analyzed for the differences between the methods. The pore-throat structure of tight sandstone was characterized by high-pressure mercury intrusion data, and the classification and evaluation standard of tight sandstone in the Ahe Formation in the Dibei Area was established combining fractal theory and physical property data. The results show that the lower physical limit porosity of the tight reservoir of the Ahe Formation in the Dibei Area is 2.4%, and the lower permeability limit is 0.021 × 10−3 μm2. According to the fractal dimension characteristics of the mercury injection curve, the different structural characteristics of four types of pores (fracture, macropore, mesopore, and small pore) can be divided with the boundary values are 3,000, 1,000, and 100 nm; the tight reservoir of the Ahe Formation in Dibei Area can be classified into four categories: (a) type I reservoir (Ф > 7%), mainly composed of fracture and macropore; (b) type II reservoir (4% < Ф < 7%), mainly made up of macropore and mesopore; (c) type III reservoir (2% < Ф < 4%), mainly formed by mesopore; and (d) type IV reservoir (Ф < 2%) dominated by small pore, followed by mesopore.
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来源期刊
Open Geosciences
Open Geosciences GEOSCIENCES, MULTIDISCIPLINARY-
CiteScore
3.10
自引率
10.00%
发文量
63
审稿时长
15 weeks
期刊介绍: Open Geosciences (formerly Central European Journal of Geosciences - CEJG) is an open access, peer-reviewed journal publishing original research results from all fields of Earth Sciences such as: Atmospheric Sciences, Geology, Geophysics, Geography, Oceanography and Hydrology, Glaciology, Speleology, Volcanology, Soil Science, Palaeoecology, Geotourism, Geoinformatics, Geostatistics.
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