天然气地质学

红柳泉—跃进地区下干柴沟组下段(E13)Ⅰ和Ⅱ砂层组的储层特征及其影响因素浅析

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  • 1.中国科学院油气资源研究重点实验室,甘肃 兰州 730000;
    2.中国科学院研究生院,北京 100049;
    3.中国石油青海油田公司勘探开发研究院,甘肃 敦煌 736202
张道伟(1972-),男,甘肃平凉人,高级工程师,在读博士,主要从事储层地质学与储层地球化学研究.

收稿日期: 2009-05-15

  修回日期: 2009-07-23

  网络出版日期: 2010-02-10

基金资助

国家科技重大专项项目(编号:2008ZX05008-|003-04);国家重点基础研究发展计划(“973”)项目(编号:2006CB202305)联合资助.

Reservoir Characteristics of Sand Beds Ⅰ and Ⅱ in Lower Member of  Xiaganchaigou Formation, Hongliuquan-Yuejin Area and Influence Factors

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  • 1.Key Laboratory of Petroleum Resources Research,Institute of Geology and Geophysics,Chinese Academy of Sciences,
    Lanzhou 730000, China; 2.Graduate University of Chinese Academy of Sciences, Beijing 100049, China;3.Research Instituteof Petroleum Exploration and Development,Qinghai Oil Field, Dunhuang 736202, China

Received date: 2009-05-15

  Revised date: 2009-07-23

  Online published: 2010-02-10

摘要

通过岩心观察、薄片鉴定、测井和录井分析,认为柴达木盆地西南红柳泉—跃进地区下干柴沟组下段(E13)Ⅰ和Ⅱ砂层组的岩石成分成熟度和结构成熟度都较低,物性都较差。红柳泉地区以岩屑长石砂岩、长石岩屑砂岩为主,发育次生孔隙,物性较差,多数属于特低孔特低渗—低孔低渗储层;而跃进地区以长石岩屑砂岩、岩屑砂岩为主,发育原生孔隙,物性相对较好,但仍以低孔低渗储层为主。影响研究区物性的因素有沉积环境、岩石类型、填隙物成分及含量、成岩改造程度。

本文引用格式

张道伟, 张顺存, 史基安 . 红柳泉—跃进地区下干柴沟组下段(E13)Ⅰ和Ⅱ砂层组的储层特征及其影响因素浅析[J]. 天然气地球科学, 2010 , 21(1) : 26 -32 . DOI: 10.11764/j.issn.1672-1926.2010.01.26

Abstract

Results of the core observation, slice identification and logging data analysis suggest that detrital rocks in sand beds Ⅰ and Ⅱ in lower member of Ganchaigou Formation, southwestern Hongliuquan-Yuejin Area are characterized by low maturity of rock composition and structure, with poor physical property. Debris-feldspar and feldspar-debris sandstones are predominate in the Hongliuquan area, with secondary porosity and poor physical property, most of which belongs to super low porosity and super low permeability reservoir-low porosity and low permeability reservoirs; while feldspar-debris and lithic sandstones are dominate in the Yuejin area, with original pore and good physical property, but which still is low porosity and low permeability reservoirs. The physical property of reservoir in this study is controlled by sedimentary environment, type rocks, composition and content of fillings, as well as degree of diagenetic reconstruction.

参考文献

[1]Dong Wenju,Shi Ji′an,Lü Zonglun,et al.Application of sublayer correlation to layer subdivision of sand members,Hongliuquan area,Qaidam basin[J]. Natural Gas Geoscience, 2007,18(4):540-544.[董文举,史基安,吕宗伦,等.小层对比在柴达木盆地红柳泉地区的应用[J].天然气地球科学,2007,18(4):540-544.]
[2]Shen Anjiang,Zhu Guohua,Shou Jianfeng,et al.A research on E13,N1,N12 clastic rock reservoir in Yuejin area,Qaidam basin,northwest China[J].Acta Sedimentologica Sinica,2001,19(1):71-78.[沈安江,朱国华,寿建峰,等.柴达木盆地跃进地区 E13、N1、N12碎屑岩储层特征[J].沉积学报,2001,19(1):71-78.]
[3]Liu Yuntian,Yang Shaoyong.Sedimentary provenances and reservoir qualities in southwestern Qaidam basin[J].Xinjiang Petroleum Geology, 2005,26(4):360-362.[刘云田,杨少勇.柴达木盆地西南地区沉积物源及储集层物性研究[J]. 新疆石油地质,2005,26(4):360-362.]
[4]Dong Wenju,Zhang Daowei,Shao Yi,et al.Sedimentary microfacies and evolution of sand membersI and Ⅱ of lower Ganchaigou Formationin Hongliuquan area of Qaidam basin[J].Natural Gas Geoscience,2009,19(1):111-115.[董文举,张道伟,邵毅,等.柴达木盆地红柳泉地区下干柴沟组E13Ⅰ和E13Ⅱ砂层组沉积微相及沉积演化研究[J].天然气地球科学,2009,19(1):111-115.]
[5]Ma Dade,Wang Shaoyi,Shou Jianfeng,et al.Sandstone reservoirs of the Palegene and Neogene in southwestern Qaidam basin[J].Journal of Palaeogeography, 2005,7(4):519-528.[马达德,王少依,寿建峰,等.柴达木盆地西南区古近系及新近系砂岩储层[J].古地理学报,2005,7(4):519-528.]
[6]Liang Changguo,Lin Chengyan, Wang Guomin,et al. Characteristics of shallow oil reservoir in Youquanzi field in western Qaidam basin[J]. Xinjiang Petroleum Geology, 2008,29(1):41-44.[梁昌国,林承焰,王国民,等.柴达木盆地西部油泉子油田浅层油藏储集层特征[J]. 新疆石油地质,2008,29(1):41-44.]
[7]Shi Yajun,Chen Yingbin,Li yanli,et al.About proposals for sandbody lithological exploration of Yuejin region in Qaidam basin[J].Natural Gas Geoscience,2006,17(5):659-662.[石亚军,陈迎宾,李延丽,等.关于柴达木盆地跃进地区岩性油气藏勘探的建议[J].天然气地球科学,2006,17(5):659-662.]
[8]Guo Feng,Chen Shiyue,Yuan Wenfang,et al.Analysis on depositional facies and reservoir of the Ganchaigou Formation,western Qaidam basin[J].Xinjiang Geology, 2006,24(1):45-52.[郭峰,陈世悦,袁文芳,等.柴达木盆地西部干柴沟组沉积相及储层分布[J].新疆地质,2006,24(1):45-52.]

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