油气地质

准噶尔盆地白家海地区三工河组储层孔隙结构及影响因素

  • 孙靖 ,
  • 王斌 ,
  • 薛晶晶
展开
  • 1.长江大学油气资源勘探技术教育部重点实验室; 2.中国石油新疆油田分公司勘探开发研究院
连小翠,1985 年生,女,长江大学在读硕士研究生,专业方向为沉积储层与成藏规律。地址:(434023)湖北省荆州市长江大学 东校区地球科学学院研究生部。E-mail:tobi221@sina.com

网络出版日期: 2011-04-20

Pore structure and influencing factors of reservoir of Sangonghe Formation in Baijiahai area, Junggar Basin

  • SUN Jing ,
  • WANG Bin ,
  • XUE Jingjing
Expand
  • 1. Key Laboratory of Exploration Technologies for Oil and Gas Resources, Ministry of Education, Yangtze University, Jingzhou 434023, China; 2. Research Institute of Petroleum Exploration and Development, Xinjiang Oilfield Company, PetroChina, Urumqi 830013, China

Online published: 2011-04-20

摘要

白家海凸起三工河组一段(J1 s1)及二段(J1s2)是侏罗系重要的勘探目的层。文中利用铸体薄片图像分析、扫描电镜、压汞分析等技术手段,对J1s1、J1s2的孔隙结构特征进行了系统分析。J1s 孔隙类型以剩余粒间孔和次生溶蚀孔为主,喉道类型以片状、弯片状及管束状为主。根据孔隙结构特征参数统计结果,将喉道划分为5 类,J1s2储层以Ⅱ类、Ⅲ类喉道为主;J1s1储层以Ⅲ类喉道为主。沉积作用和成岩作用是影响研究区储层物性的主要因素,且成岩作用中的胶结作用和溶蚀作用的影响最大。

本文引用格式

孙靖 , 王斌 , 薛晶晶 . 准噶尔盆地白家海地区三工河组储层孔隙结构及影响因素[J]. 岩性油气藏, 2011 , 23(2) : 35 -40 . DOI: 10.3969/j.issn.1673-8926.2011.02.007

Abstract

The first and second members of Sangonghe Formation in Baijiahai area are the important exploration target zones. The cast thin section, scanning electronic microscope, cast image analysis and mercury injection analysis are applied to analyze the pore structure of Sangonghe Formation reservoir in Baijiahai area. The main pores of Sangonghe Formation are residual primary intergranular pore and secondary dissolved pore. The throat types are lamellar or curved lamellar and bundle tubular. Based on the result of pore structure calculation, the throats are divided into five types. The throats of the second member of Sangonghe Formation are mainly typeⅡ and Ⅲ, and the throats of the first member of Sangonghe Formation are type Ⅲ throat. The main influencing factors of the pore structure are sedimentation and diagenesis, and the cementation and dissolution are dominant factors.

参考文献

[1] 况军,唐勇,朱国华,等.准噶尔盆地侏罗系储集层的基本特征及其主控因素分析[J].石油勘探与开发,2002,29(1):52-60.
[2] 王敏芳,焦养泉,张福顺,等.准噶尔盆地侏罗系储集层特征及影响因素分析[J].大庆石油地质与开发, 2005,24(5):20-24.
[3] 王卓飞,蒋宜勤,祝嗣全.准噶尔盆地侏罗系低渗透油气储层特征及成因探讨[J].断块油气田,2003,10(5):23-36.
[4] 沙文武,邵江,郭耀华.镇泾地区三叠系延长组储层评价[J].天然气工业, 2001,21(增刊):35-39.
[5] 卫平生,谭开俊,魏郑铁.巴彦浩特盆地石炭系储层特征及成岩作用[J].天然气地球科学,2008,19(5):581-586.
[6] 刘国超.伊通盆地莫里青断陷双阳组水下扇储层特征及控制因素[J].岩性油气藏,2009,21(3):40-44.
[7] 谢武仁,杨威,杨光,等.川中地区上三叠统须家河组砂岩储层孔隙结构特征[J].天然气地球科学,2010,21(3):435-439.
[8] 刘林玉,王震亮.白豹地区延长组长3 储层的成岩作用与成岩相[J].西北大学学报:自然科学版,2008,38(1):99-102.
[9] 禚喜准,王琪,陈国俊,等.恩平凹陷恩平组下段成岩过程分析与储层动态评价[J].沉积学报,2008,26(2):257-282.
[10] 黄龙,田景春,肖玲,等.鄂尔多斯盆地富县地区长6 砂岩储层特征及评价[J].岩性油气藏,2008,20(1):83-87.
[11] 徐樟有,宋丽,吴欣松,等.川中地区上三叠统须家河组典型气藏解剖与天然气成藏主控因素分析[J].岩性油气藏,2009,21(2):7-11.
[12] 龙玉梅. 鄂尔多斯盆地坪北油田上三叠统延长组成岩作用及孔隙结构[D].西安:西北大学,2002.
[13] 袁静.松辽盆地东南隆起区上侏罗统孔隙特征及影响因素[J].煤田地质与勘探,2004,32(2):7-10.
[14] 李少华,陈新民,龙玉梅,等.坪北油田储层成岩作用与孔隙演化[J].沉积与特提斯地质,2002,22(3):25-29.
[15] 刘孟慧,赵澄林.碎屑岩储层成岩演化模式[M].东营:石油大学出版社,1993:48-51.
文章导航

/