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塔里木盆地孔雀河斜坡志留系致密砂岩储层特征及主控因素
石油实验地质
2013年 35卷 第6期
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Title
Characteristics and main controlling factors of tight sandstone reservoirs in Silurian of Kongquehe slope, Tarim Basin
作者
王斌
赵永强
王恕一
张根法
罗宇
陈绪云
雷蕾
Authors
Wang Bin
Zhao Yongqiang
Wang Shuyi
Zhang Genfa
Luo Yu
Chen Xuyun
Lei lei
单位
中国石油化工股份有限公司 石油勘探开发研究院 无锡石油地质研究所,江苏 无锡 214126
中国石油化工股份有限公司 西北油田分公司 勘探开发研究院,乌鲁木齐 830011
北京华油光大能源技术有限公司,北京 100029
Organization
Wuxi Research Institute of Petroleum Geology, SINOPEC, Wuxi, Jiangsu 214126, China
Research Institute of Exploration and Development, SINOPEC Northwest Oilfield Company, Urumqi, Xinjiang 830011, China
Beijing China-Petroleum Everbright Energy Technology Co Ltd, Beijing 100029, China
摘要
综合利用岩心、薄片、铸体薄片、扫描电镜和物性分析等资料,对塔里木盆地孔雀河斜坡志留系储层特征进行了总结,从碎屑组分、沉积和成岩等多方面分析了储层发育的主控因素。研究结果表明:研究区志留系储层的岩石类型以岩屑砂岩、长石岩屑砂岩为主,结构成熟度中等,成分成熟度较低。物性总体较差,属于低孔—特低孔、特低渗的致密砂岩储层,储集空间主要为粒间溶孔、粒内溶孔和微裂缝,孔喉连通性差。沉积作用是控制志留系砂岩储层形成的基础;强烈的压实作用和普遍的胶结作用是致密砂岩储层形成的关键因素;构造破碎作用和溶蚀作用是形成储层次生孔隙的重要因素。
Abstract
The sandstone reservoir characteristics such as clastic component, sedimentation, diagenesis and so on in the Silurian of Kongquehe slope were analyzed based on the data of core, casting film, electron microscope scanning and reservoir property analysis to determine the main controlling factors of reservoir quality. The research result shows that reservoir lithology is mainly lithic sandstone and feldspathic litharenite, which have medium texture maturity and lower maturity composition. Reservoir accumulation properties are worse, which belong to low-porosity and extra-low-permeability tight sandstone reservoirs. Main reservoir space is corrosion pore between grains or in grains and a few micro-fractures. The connectivity between pore space and throat is poor. Sedimentation is the fundamental factor for the development of sandstone reservoirs in Silurian. Strong compaction and widespread cementation are the dominant factors. Structure fracturing and dissolution are also important factors for the formation of secondary pores in sandstone reservoirs.
关键词:
致密砂岩;
储层特征;
主控因素;
志留系;
孔雀河斜坡;
塔里木盆地;
DOI
https://doi.org/10.11781/sysydz201306615