自然科学版
陕西师范大学学报(自然科学版)
资源与环境科学
储层沉积-成岩作用的物性响应特征
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时建超1, 孙卫1, 张创2, 莫建武3, 丁磊2,张奉1
(1 西北大学 大陆动力学国家重点实验室,陕西 西安 710069;2 陕西延长石油(集团)有限责任公司研究院,陕西 西安 710069;3 中原油田分公司勘探开发科学研究院,河南 濮阳 457001)
时建超,男,博士研究生,主要从事油气储层地质方面研究.E-mail:jcshi@sohu.com.
摘要:
对苏北盆地沙埝油田阜三段(E1f3)储层岩石特征、物性特征、成岩作用及孔隙演化过程进行研究,在此基础上分析沉积和成岩作用对储层物性的控制作用,用数理统计方法对相关的影响因素进行了定量分析.研究表明:储层物性明显受沉积相带和成岩作用控制,由水下分流河道、河口砂坝到席状砂,物性依次变差;压实过程损失的孔隙度为13.3%,早期石英次生加大与碳酸盐胶结损失孔隙度9.5%,长石、岩屑及填隙物溶蚀增加孔隙度11.9%,晚期石英次生加大与碳酸盐胶结损失孔隙度9.7%;胶结作用造成的孔隙损失大于压实作用;对本区物性影响较大的沉积-成岩因素为粒度、压实作用、胶结作用和溶蚀作用.
关键词:
沉积作用;成岩作用;物性;苏北盆地
收稿日期:
2012-09-05
中图分类号:
TE122.2
文献标识码:
A
文章编号:
1672-4291(2013)02-0088-06
基金项目:
国家科技支撑计划项目(2007BAB17B00).
Doi:
Physical property response characteristics to sedimentation and diagenesis of reservoir
SHI Jian-chao1, SUN Wei1, ZHANG Chuang2, MO Jian-wu3,DING Lei2, ZHANG Feng1
(1 Key Laboratory of Continental Dynamics of Ministry of Education, Northwest University, Xi′an 710069, Shaanxi, China;2 Yanchang Petroleum Group Research Institute, Xi′an 710069, Shaanxi, China; 3 Exploration and Development Research Institute, Zhongyuan Branch Company of SINOPEC, Puyang 457001, Henan, China)
Abstract:
The rock characteristics, physical property, diagenesis and the process of porosity evolution are analysed in E1f3 reservoir of Shanian oilfield, Subei basin. On the basis,the control action of physical property from sedimentation and diagenesis is analysed,and the related factors are quantitatively analyzed by mathematical statistics method.The research shows that physical property is obviously controlled by sedimentary microfacies and diagenesis, and from subsea distributary channel, mouth bar to sheet, physical properties become worse. The porosity decreases 13.3% by compaction, 9.5% by quartz secondary outgrowth and carbonatite cementation in early phase, and increases 11.9% by feldspar, debris and interstitial material corrosion, and decreases 9.7% by hydrosialite, quartz secondary outgrowth, and ankerite cementation and metasomasis in late phase. The main control factors of physical property in study area are clast size, compaction, cementation and corrosion.
KeyWords:
sedimentation; diagenesis; physical property; Subei basin