鄂尔多斯盆地富县地区延长组长6储层特征

张惠; 孟祥振; 郭艳琴; 张晓泉; 杨华; 刘艳; 冯辉

doi:10.11781/sysydz201003242

鄂尔多斯盆地富县地区延长组长6储层特征

doi: 10.11781/sysydz201003242

张惠^1,2,
孟祥振³,
郭艳琴²,
张晓泉³,
杨华³,
刘艳³,
冯辉³

1.
西北大学, 地质学系, 西安, 710069
2. 西安石油大学, 油气资源学院, 西安, 710065
3. 延长油田股份有限公司, 陕西, 延安, 717111

基金项目: 国家科技重大专项专题(2008ZX05005-004-08HZ);国家自然科学基金项目(40902042)联合资助

详细信息

作者简介:
张惠(1976- ),女,博士,讲师,主要从事石油地质研究.E-mail:zhanghui0911@263.net.

中图分类号: TE122.23
计量
- 文章访问数: 1728
- HTML全文浏览量: 82
- PDF下载量: 951
- 被引次数: 0
出版历程
- 收稿日期: 2010-03-10
- 修回日期: 2010-05-10
- 刊出日期: 2010-06-28

CHARACTERISTICS OF THE CHANG 6 RESERVOIR OF THE FUXIAN AREA IN THE ORDOS BASIN

1.
Department of Geology, Northwest University, Xi'an, Shaanxi 710069, China
2. College of Oil and Gas Resources, Xi'an Shiyou University, Xi'an, Shaanxi 710065, China
3. Yanchang Oilfield Co. Ltd. , Yan'an, Shaanxi 717111, China

摘要

摘要: 鄂尔多斯盆地富县地区长6油层组主要发育三角洲沉积,其中分流河道和水下分流河道是主要的油气储集层。长6油层组储集层岩石类型以岩屑长石细砂岩和长石细砂岩为主,颗粒间多为线、点—线接触,孔隙和薄膜式胶结,总体具有成分成熟度低、结构成熟度高的特征。粒间孔和长石溶孔是主要的储集空间,其中以小孔和微孔为主,渗透率小于3×10^-3μm²,为特低渗储层和接近致密储层。研究区较强的压实作用、胶结作用是形成低孔低渗的主要因素,而溶蚀作用是储层物性改善的主要因素。
- 成岩作用 /
- 储层特征 /
- 延长组 /
- 富县地区 /
- 鄂尔多斯盆地
Abstract: Delta sediments are the main deposits in the Chang 6 oil beds of Yanchang Formation in Fuxian area of the Ordos Basin and the sand bodies of distributary channel and subaquatic distributary channels are main reservoirs for the hydrocarbon.Fine lithic arkose sandstone and fine arkose sandstone are main sandstones of the Chang 6 reservoir.They have line and point-line contact forms with pore and thin film cementation between rock grains.The Chang 6 reservoir is characterized by the low component maturity and high textural maturity.The main pore types are granular pore and secondary feldspar-dissolution pore which are mainly composed of small hole and micropore.The Chang 6 reservoir has super low permeability and is accessed densify reservoir of which the permeability is less than 3×10^-3μm².The strong compaction and cementation are the main factors which cause the low porosity and low permeability of the reservoir,while dissolution is the main factor for improving the physical property of the reservoir.
- diagenesis /
- reservoir characteristic /
- Yanchang Formation /
- Fuxian area /
- Ordos Basin

HTML全文

参考文献(11)

[1]	郭艳琴.富县探区延长组储层微观特征研究[D].西安:西北大学,2006.
[2]	谢正温,谢渊,王剑,等.鄂尔多斯盆地富县地区延长组主要油层组储层特征[J].石油实验地质,2005,27(6):575-582.
[3]	吴胜和,熊琦华.油气储层地质学[M].北京:石油工业出版社,1997:25.
[4]	文玲,胡书毅,田海芹.靖安油田延长组长6段低孔低渗透储层特征及评价[J].西北地质,2001,34(4):53-60.
[5]	方少仙,侯方浩.石油天然气储层岩石学[M].东营:中国石油大学出版社,2006:158.
[6]	PAXTON S T,SZABO J O,CALVERT C S,et al.Preservation of primary porosity in deeply buried sandstones:A new play concept from the Cretaceous Tuscaloosa Sandstone of Louisiana[J].AAPG Bulletin,1990,74(5):737.
[7]	SZABO J O,PAXTON S T.Intergranular volume(1GV)decline curves for evaluating and predicting compaction and porosity loss in Sandstones[J].AAPG Bulletin,1991,75(3):678.
[8]	郭艳琴,王起琮,庞军刚,等.安塞油田长2、长3浅油层成岩作用及孔隙结构特征[J].西北大学学报(自然科学版),2007,37(3):443-448.
[9]	SURDAM R C,CROSSEY L J,HAGEN E S,et al.Organic-inorganic interaction and sandstone diagenesis[J].AAPG Bulletin,1989,78(1):1-23.
[10]	王琪,史基安,薛莲花,等.碎屑储集岩成岩演化过程中流体-岩石相互作用特怔:以塔里木盆地西南坳陷地区为例[J].沉积学报,1999,17(4):584-590.
[11]	袁静,赵澄林.水介质的化学性质和流动方式对深部碎屑岩储层成岩作用的影响[J].石油大学学报(自然科学版),2000,24(1):60-63.