伊朗扎格罗斯盆地白垩质灰岩储层特征及开发建议

徐德军; 张文才; 杜秀娟; 李艳军; 苏瑜

doi:10.11781/sysydz201001015

伊朗扎格罗斯盆地白垩质灰岩储层特征及开发建议

doi: 10.11781/sysydz201001015

1.
中国石油大学(华东)地球资源与信息学院, 山东, 东营, 257061
2. 中国石化集团国际石油勘探开发有限公司, 北京, 100083
3. 中国石油化工股份有限公司, 石油勘探开发研究院, 北京, 100083

详细信息

作者简介:
徐德军(1967- ),男,博士生,高级工程师,从事油气田开发地质、开发工艺研究工作.E-mail:djxu@sipc.cn.

中图分类号: TE122.23
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出版历程
- 收稿日期: 2009-09-26
- 修回日期: 2009-12-18
- 刊出日期: 2010-02-28

RESERVOIR CHARACTERISTICS AND DEVELOPMENT SUGGESTION OF CHALKY LIMESTONE IN THE ZAGROS BASIN, IRAN

1.
College of Geo-Resources and Information, China University of Petroleum, Dongying, Shandong 257061, China
2. Sinopec International Petroleum Exploration and Petroleum Corporation, Beijing 100083, China
3. Exploration and Production Research Institute, SINOPEC, Beijing 100083, China

摘要

摘要: 伊朗Y油田含油层系Sarvak组油气储集层主要为富含蛤类化石的白垩质灰岩,储集空间类型主要为孔隙和洞,为中孔低渗—特低渗型储层。沉积环境为浅海碳酸盐岩台地边缘斜坡及礁边缘相。储层层内相对均质,而层间非均质性严重。优质储层受沉积环境和成岩作用双重因素控制,发生白垩化成岩作用较强的碳酸盐岩台地前缓坡相和台地浅滩相是白垩质灰岩储层发育的有利相带。Sarvak组油藏类型为层状边水油藏,油水界面倾斜,开发中尽可能依托储层特征及油藏类型,增加开发效益。
- 储层特征 /
- 沉积环境 /
- 白垩质灰岩 /
- Sarvak组 /
- 扎格罗斯盆地 /
- 伊朗
Abstract: Reservoirs of Sarvak Formation in the Y Oilfield of the Zagros Basin,Iran are rich rudist-bearing chalky limestone.Reservoir spaces are mainly porosities and vuggs,with few fractures.The reservoirs were deposited in slope of marginal neritic carbonate platform and marginal reefs.The heterogeneity in intralayer is weak while strong in interlayer.In charge of sedimentary environment and diagenesis,high-quality reservoirs developed in slope of marginal neritic carbonate platform and marginal reefs which with slightly chalk-diagenesis.Sarvak Formation is a multi-layer stacked reservoir with weak edge water and a tilted oil-water contact.Development must depend on reservoir characteristics and reservoir types.
- reservoir characteristics /
- sedimentary environment /
- chalky limestone /
- Sarvak Formation /
- Zagros Basin /
- Iran

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参考文献(14)

[1]	PITTMAN E D.Microporosity in carbonate rocks[J].AAPG Bulletin,1971,85:1873-1881.
[2]	LOUCKS R G,SARG J F.Carbonate Sequence Stratigraphy:Recent Development and Applications:AAPG Memoir 57[M].Tulsa:AAPG Press,1993:545.
[3]	JAMES N P.Reefs[M].//WALKER R G.Facies Models:Geoscience Canada:Reprint Series 1.1984:229-244.
[4]	LUCIA F J.Rock-fabric/petrophysical classification of carbonate pore space for reservoir characterization[J].AAPG Bulletin,1995,79:1275-1300.
[5]	MOORE C H.Carbonate Diagenesis and Porosity,Developments in Sedimentology 46[M].Amsterdam:Elsevier,1989:338.
[6]	杨宁,吕修祥,陈梅涛,等.塔里木盆地轮南、塔河油田碳酸盐岩储层特征研究:以沙107井和轮古40井为例[J].石油实验地质,2008,30(3):247-251.
[7]	胡新铭,金平信,刘承红.渤南洼陷渤深6碳酸盐岩潜山储层描述[J].油气地质与采收率,2006,13(4):31-33.
[8]	KENT P E,SLINGER F C,THOMAS A N.Stratigraphical Exploration Surveys in South-West Persia[C].Proc Third World Petroleum Congress Sect I.1951:64-75.
[9]	苏崇华.疏松砂岩油田生产过程中储层伤害机理研究[J].中国海上油气,2009,21(1):31-34.
[10]	蒋小琼,范明,王恕一,等.埋藏成岩环境碳酸盐岩溶蚀作用模拟实验研究[J].石油实验地质,2008,30(6):643-646.
[11]	张奎华,马立权.济阳坳陷下古生界碳酸盐岩潜山内幕储层再研究[J].油气地质与采收率,2007,14(4):26-28.
[12]	阎相宾.塔河油田奥陶系碳酸盐岩储层特征[J].石油与天然气地质,2002,23(3):262-265.
[13]	肖玉茹,何峰煜,孙义梅.古洞穴型碳酸盐岩储层特征研究:以塔河油田奥陶系古洞穴为例[J].石油与天然气地质,2003,24(1):75-86.
[14]	孟元林,吴巍,姜文亚,等.双清地区储层异常高孔带分布特征与成因分析[J].中国海上油气,2008,20(3):148-151.