川中北部侏罗系大安寨段湖相碳酸盐岩储层特征研究

Du Jiangmin, Zhang Xiaoli, Yu Yanqiu, Huang Kaiwei, Guo Hongguang, Zhong Gaorun, Yu Bowei, Z. Yuanyuan
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引用次数: 1

摘要

根据川中北部下侏罗统大安寨段岩心宏观和微观特征,结合物性资料,对储层岩性特征、物性特征、储层空间类型等储层特征及储层发育控制因素进行了详细研究。研究认为,储层有两种典型类型:结晶壳灰岩和泥质壳灰岩。储层物性差,超低孔低渗,可通过裂缝明显改善储层物性。储集空间类型为孔隙-裂缝型,以微裂缝为主,并伴有溶蚀孔隙。储层发育受沉积作用、成岩作用和构造作用共同控制。贝壳滩和湖坡是储层发育的有利相。溶蚀作用是提高储层孔隙度和渗透率的主要构造成岩作用。构造裂缝是储层高效、高产的必要条件。关键词:控制因素,大安寨段,下侏罗统,川中北部,储层特征
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Lacustrine Carbonate Reservoir Characteristics Research of JurassicDa’anzhai Member in North Central Sichuan Basin
Based on both macroscopic and microscopic characteristics of cores from Lower Jurassic Da'anzhai Member in north central Sichuan Basin, and combined with physical property data, a detail study has been conducted, which includes reservoir characteristics such as lithologic characters, physical properties, and reservoir space types, and control factors of reservoir development. The study suggests that, there are two typical kinds of reservoirs: crystalline shell limestone and argillaceous shell limestone. The reservoirs properties are poor with ultra-low porosity and low permeability, which can be significantly improved by fractures. Reservoir space type is pore-fracture, mainly constitutive of the micro-fractures accompanied by dissolved pores. The reservoir development is controlled by sedimentation, diagenesis and tectogenesis together. Shell beach and lacustrine slop are the favorable facies for reservoir development. Dissolution is the primary constructive diagenesis to improve reservoir porosity and permeability. Structural fractures are necessary for reservoir ef- fectiveness and high production. Keyword: Control factor, Da'anzhai member, lower Jurassic, north central Sichuan Basin, reservoir characteristics.
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