• 中国出版政府奖提名奖

    中国百强科技报刊

    湖北出版政府奖

    中国高校百佳科技期刊

    中国最美期刊

    留言板

    尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

    姓名
    邮箱
    手机号码
    标题
    留言内容
    验证码

    湖相致密白云岩不均一油藏特征及主控因素

    姚悦 王刚 李乐 刘永河

    姚悦, 王刚, 李乐, 刘永河, 2017. 湖相致密白云岩不均一油藏特征及主控因素. 地球科学, 42(12): 2327-2335. doi: 10.3799/dqkx.2017.145
    引用本文: 姚悦, 王刚, 李乐, 刘永河, 2017. 湖相致密白云岩不均一油藏特征及主控因素. 地球科学, 42(12): 2327-2335. doi: 10.3799/dqkx.2017.145
    Yao Yue, Wang Gang, Li Le, Liu Yonghe, 2017. The Reservoir Heterogeneity Characteristics and Affecting Factors of Tight Lacustrine Dolomite Reservoirs. Earth Science, 42(12): 2327-2335. doi: 10.3799/dqkx.2017.145
    Citation: Yao Yue, Wang Gang, Li Le, Liu Yonghe, 2017. The Reservoir Heterogeneity Characteristics and Affecting Factors of Tight Lacustrine Dolomite Reservoirs. Earth Science, 42(12): 2327-2335. doi: 10.3799/dqkx.2017.145

    湖相致密白云岩不均一油藏特征及主控因素

    doi: 10.3799/dqkx.2017.145
    基金项目: 

    “十三五”国家油气专项“近海大中型油气田形成条件及勘探技术” 2016ZX05024-006

    中国石油股份有限公司大港油田重点项目“塘沽地区沙三5特殊岩性体沉积特征及油藏综合评价” DGYT-2012-JS-566

    详细信息
      作者简介:

      姚悦(1992-), 女, 在读研究生, 主要从事油气储层预测研究

    • 中图分类号: P618.13

    The Reservoir Heterogeneity Characteristics and Affecting Factors of Tight Lacustrine Dolomite Reservoirs

    • 摘要: 渤海湾盆地塘沽地区沙三5亚段发育湖相含油泥质白云岩层系,油藏顶面埋深2 800~3 600 m,属于中深-深层的断块-岩性油藏,储层为致密裂缝白云岩.本文通过岩心观察、实验室分析、压力测试、裂缝分析等手段,重点研究了致密白云岩储层岩石相、储集性、复杂含油性和油藏不均一性特征,分析了成藏主控因素及成藏模式.研究表明:储层岩性以白云岩、泥质白云岩为主,为中-低孔、低渗-特低渗的裂缝-孔隙型储层,储集空间主要为晶间孔、溶孔、裂缝及溶缝;超压与含油性密切相关,超压断块井均中高产、含水率低于20%且呈持续降低趋势,常压断块井均低产、含水率高于55%且稳定-上升趋势;白云岩层系内厚层泥岩为优质烃源岩,提供充足油源;断层封闭性控制油气聚集,进而控制生烃型超压的分布,超压成为油气富集的重要标志;油气充注晚于断块-岩性圈闭形成时间,使油气充注有效.

       

    • 图  1  塘沽地区沙三5段顶面构造、井位分布及生产特征图

      赵耀等(2016)修改

      Fig.  1.  Top surface structure map with wells position and producting properties of Es35 in Tangguo area

      图  2  沙三5亚段泥质白云岩油藏剖面简化图

      Fig.  2.  Dolomite eservoir section of ES3-5

      图  3  岩石相类型与裂缝特征素描

      Fig.  3.  Fracture properties and lithologic types sketch

      图  4  白云岩储集空间特征

      a.豆状溶孔,白云岩,3 144.96 m;b.针状溶孔,白云岩,3 142.31 m;c.晶间孔,SEM图像,泥质白云岩,3 121.70 m(资料来自南京大学);d.方沸石充填的微裂缝,单偏光,10×5倍,泥质白云岩,3 131.05 m;e.藻纹层与针状溶孔,白云岩,3 151.12 m;f.变形藻纹层与针状溶孔,白云岩,3 152.31 m;g.藻纹层与石英长石碎屑层,单偏光,10×5倍,白云岩,3 160.39 m;h.藻纹层与泥质纹层,单偏光,10×10倍,白云岩,3 143.17 m

      Fig.  4.  Reservoir space of dolomite rock

      图  5  试采井的综合含水率变化趋势

      Fig.  5.  Water cut rate in test wells

      图  6  亲油层的油水赋存状态模式图

      Fig.  6.  Oil and water occurrence state in oil-wet reservoir

      图  7  有机质类型、成熟度(a)及烃源岩评价(b)

      Fig.  7.  Organic matter type, maturity (a), and the evaluation of the hydrocarbon source rocks (b)

      图  8  裂缝发育程度与岩性关系图

      Fig.  8.  Fracture density and lithologic types diagram

      图  9  沙三5亚段泥质白云岩油藏成藏模式图

      Fig.  9.  Oil accumulation pattern of dolomite reservoir in Es35

    • [1] Arribas, M.E., Bustillo, A., Tsige, M., 2004.Lacustrine Chalky Carbonates; Origin, Physical Properties and Diagenesis (Palaeogene of the Madrid Basin, Spain).Sedimentary Geology, 166(3-4):335-351.doi: 10.1016/j.sedgeo.2004.01.012
      [2] Christopher, A.S., 2008.Lacustrine Basins as Mixed Siliciclastic-Carbonate Systems, Examples from the East African Rif.Geological Society of America, 40(6):95. https://gsa.confex.com/gsa/2008AM/finalprogram/session_21541.htm
      [3] Deng, R.J., Xu, B., Qi, J.F., et al., 2006.Sedimentation Characteristics and Factors Affecting the Reservoir in Palaeogene Shasan Member of Beitang Sag, Huanghua Depression.Acta Petrologica et Mineralogica, 25(3):230-236(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSKW200603007.htm
      [4] Deng, R.J., Chai, G.Q., Yang, H., et al., 2001.Forming Conditions and Distribution Characteristics of Tertiary Oil and Gas Pools in Beitang Sag.Petroleum Exploration and Development, 28(1):27-29(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-SKYK200101008.htm
      [5] Deng, R.J., Xu, B., Qi, J.F., et al., 2005.Petroleum Geological Role of Paleogene Overpressure Reservoirs in Tanggu-Xincun of Beitang Sag, Bohai Bay Basin.Petroleum Exploration and Development, 32(6):46-51(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-SKYK200506010.htm
      [6] Du, Y.H., 1990.Eogene Lacustrine Carbonate Rocks and Sedimentary Model in Bohai Bay Region.Oil & Gas Geology, 11(4):376-392+465-466 (in Chinese with English abstract).
      [7] Feng, Y.L., Zhang, Y.J., Wang, R.J., et al., 2011.Dolomites Genesis and Hydrocarbon Enrichment of the Fengcheng Formation in the Northwestern Margin of Junggar Basin.Petroleum Exploration and Development, 38(6):685-692(in Chinese with English abstract). https://www.researchgate.net/publication/281925063_Dolomites...
      [8] Feng, Y.L., Zhou, H.M., Ren, J.Y., et al., 2010.Paleogene Sequence Stratigraphy in the East of the Bohai Bay Basin and Its Response to Structural Movement.Science China:Science Terrae, 40(10):1356-1376(in Chinese).
      [9] Jia, C.Z., Zou, C.N.Li, J.Z., et al., 2012.Assessment Criteria, Mmain Types, Basic Features and Resource Prospects of the Tight Oil in China.Acta Petrolei Sinica, 33(3):343-350(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SYXB201203000.htm
      [10] Kuang, L.C., Tang, Y., Lei, D.W., et al., 2012.Formation Conditions and Exploration Potential of Tight Oil in the Permian Saline Lacustrine Dolomitic Rock, Junggar Basin, NW China.Petroleum Exploration and Development, 39(6):657-667(in Chinese with English abstract). https://www.sciencedirect.com/science/article/pii/S1876380412600950
      [11] Li, M.G., Qi, J.F., Yang, Q., et al., 2009.Cenozoic Structure Features of Huanghua Depression and its Structure Dynamics Model.Acta Geoscientia Sinica, 30(2):201-209(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQXB200902009.htm
      [12] Li, L., Yao, G.Q., Liu, Y.H., et al, 2015a.Characteristics of Analcime-Dolomite Reservoir from Shahejie Formation in Well Tang10 Block of Danggang Oilfield.Acta Petroleum Sinica, 36(10), 1210-1220 (in Chinese with English abstract). http://d.wanfangdata.com.cn/Periodical_syxb201510004.aspx
      [13] Li, L., Yao, G.Q., Liu, Y.H., et al, 2015b.Major and Trace Elements Geochemistry and Geological Implications of Dolomite-Bearing Mudstones in Lower part of Shahejie Formation in Tanggu Area, Eastern China.Earth Science, 40(9):1480-1496 (in Chinese with English abstract). http://industry.wanfangdata.com.cn/dl/Detail/Periodical?id=...
      [14] Lin, P.X., Lin, C.M., Yao, Y., et al, 2017.Characteristics and Causes of Analcime Distributed in Dolostone of the Member 3 of Paleogene Shahejie Formation in Beitang Sag, Bohai Bay Basin.Journal of Palaeogeography, 19(2):241-256 (in Chinese with English abstract). https://es.scribd.com/doc/221791959/AAPG-Memoir-69-Reservoir...
      [15] Lomando, A.J., 1996.Exploration for Lacustrine Carbonate Reservoirs:Insights from West Africa:ABSTRACT.AAPG Bulletin, 80:(8):1308-1309.doi: 10.1306/64ed93d0-1724-11d7-8645000102c1865d
      [16] Luo, Q., 2002.Fault Controlling Hydrocarbon Theory and Petroleum Exploration Practice.Earth Science, 27(6):751-756(in Chinese with English abstract). http://www.nsfc.gov.cn/Portals/0/fj/english/fj/pdf/2009/021.doc
      [17] Sarg, J.F., Suriamin, N., Tìnavsuu-Milkeviciene, K., et al., 2013.Lithofacies, Stable Isotopic Composition, and Stratigraphic Evolution of Microbial and Associated Carbonates, Green River Formation (Eocene), Piceance Basin, Colorado.AAPG Bulletin, 97(11):1937-1966.doi: 10.1306/07031312188
      [18] Sun, Y., Zhong, J.H., Yuan, X.C., et al., 2008.Review and Prospect of the Study on Domestic Lacustrine Carbonate Rocks.Special Oil & Gas Reservoirs, 15(5):1-6(in Chinese with English abstract). http://d.wanfangdata.com.cn/Periodical_tzyqc200805001.aspx
      [19] Wang, J.Z., Xiang, C.F., Pang, X.Q., 2013.Faultsealing Mechanisms in the Carbonate Sequence.Journal of China University of Mining & Technology, 42(4):616-624(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZGKD201304016.htm
      [20] Wu, X.L., Gao, B., Ye, X., et al., 2013.Shale Oil Accumulation Conditions and Exploration Potential of Faulted Basins in the East of China.Oil & Gas Geology, (4):455-462(in Chinese with English abstract). https://www.researchgate.net/publication/286883342_Shale_oil...
      [21] Yu, Z.C., ,Liu, L., Sun, X.M., et al.2012.Evidence of Paleogene Thermal Fluid Activities and Their Impact on Porosity-Permeability of Reservoir in Qikou Sag.Journal of Jilin University(Earth Science Edition), 42(Sup.3):1-13(in Chinese with English abstract). https://www.researchgate.net/publication/286279509_Evidence_of...
      [22] Zhao, Y., Yao, G.Q., Mu, l.H., et al., 2016.Characteristics and Controlling Factors of Fractures in Lacustrine Dolostones Reservoirs in Tanggu District.Earth Science, 41(2):252-264(in Chinese with English abstract).
      [23] Zhou, L.H., Lu, Y., Xiao, D.Q., et al., 2011.Basinal Texture Structure of Qikou Sag in Bohai Bay Basin and its Evolution.Natural Gas Geoscience, 22(3):373-382(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-TDKX201103002.htm
      [24] Zhou, S.X., 1992.The Research Status of the Study on Domestic Lacustrine Carbonate Rocks.Oil & Gas Geology, 13(4):461-462(in Chinese with English abstract).
      [25] 邓荣敬, 柴公权, 杨桦, 等, 2001.北塘凹陷第三系油气藏形成条件与油气分布.石油勘探与开发, 28(1):27-29. http://www.cnki.com.cn/Article/CJFDTOTAL-SKYK200101008.htm
      [26] 邓荣敬, 徐备, 漆家福, 等, 2005.北塘凹陷塘沽-新村地区古近系异常高压特征及其石油地质意义.石油勘探与开发, 32(6):46-51. http://www.cnki.com.cn/Article/CJFDTOTAL-SKYK200506010.htm
      [27] 邓荣敬, 徐备, 漆家福, 等, 2006.北塘凹陷古近系沙河街组三段沉积特征及储层的影响因素.岩石矿物学杂志, 25(3):230-236. http://www.oalib.com/paper/4339297
      [28] 杜韫华, 1990.渤海湾地区下第三系湖相碳酸盐岩及沉积模式.石油与天然气地质, 11(4):376-392+465-466. doi: 10.11743/ogg19900404
      [29] 冯有良, 张义杰, 王瑞菊, 等, 2011.准噶尔盆地西北缘风城组白云岩成因及油气富集因素.石油勘探与开发, 38(6):685-692. http://www.cnki.com.cn/Article/CJFDTOTAL-SKYK201106006.htm
      [30] 冯有良, 周海民, 任建业, 等.2010.渤海湾盆地东部古近系层序地层及其对构造活动的响应.中国科学:地球科学, (10):1356-1376. http://www.oalib.com/paper/4153154
      [31] 贾承造, 邹才能, 李建忠, 等, 2012.中国致密油评价标准、主要类型、基本特征及资源前景.石油学报, 33(3):343-350. doi: 10.7623/syxb201203001
      [32] 匡立春, 唐勇, 雷德文, 等, 2012.准噶尔盆地二叠系咸化湖相云质岩致密油形成条件与勘探潜力.石油勘探与开发, 39(6):657-667. http://www.cnki.com.cn/Article/CJFDTOTAL-SKYK201206004.htm
      [33] 李乐, 姚光庆, 刘永河, 等, 2015a.大港油田塘10井区沙河街组方沸石白云岩储层特征.石油学报, 36(10):1210-1220. http://www.cnki.com.cn/Article/CJFDTOTAL-SYXB201510004.htm
      [34] 李乐, 姚光庆, 刘永河, 等, 2015b.塘沽地区沙河街组下部含云质泥岩主微量元素地球化学特征及地质意义.地球科学, 40(9) 1480-1496. http://www.earth-science.net/WebPage/Article.aspx?id=3152
      [35] 李明刚, 漆家福, 杨桥, 等, 2009.渤海湾盆地黄骅坳陷新生代结构特征及构造动力学模式.地球学报, 30(2):201-209. http://d.wanfangdata.com.cn/Periodical/dqxb200902007
      [36] 林培贤, 林春明, 姚悦, 等, 2017.渤海湾盆地北塘凹陷古近系沙河街组三段白云岩中方沸石的特征及成因.古地理学报, 19 (2):241-256. doi: 10.7605/gdlxb.2017.02.019
      [37] 罗群, 2002.断裂控烃理论与油气勘探实践.地球科学, 27(6):751-756. http://www.earth-science.net/WebPage/Article.aspx?id=1198
      [38] 孙钰, 钟建华, 袁向春, 等, 2008.国内湖相碳酸盐岩研究的回顾与展望.特种油气藏, 15(5):1-6. http://d.wanfangdata.com.cn/Periodical_tzyqc200805001.aspx
      [39] 王建忠, 向才富, 庞雄奇, 2013.碳酸盐岩层系断层封闭机理研究.中国矿业大学学报, 42(4):616-624. http://www.wenkuxiazai.com/doc/b10ce107a300a6c30c229f85.html
      [40] 武晓玲, 高波, 叶欣, 等, 2013.中国东部断陷盆地页岩油成藏条件与勘探潜力.石油与天然气地质, (4):455-462. doi: 10.11743/ogg20130405
      [41] 于志超, 刘立, 孙晓明, 等, 2012.歧口凹陷古近纪热流体活动的证据及其对储层物性的影响.吉林大学学报(地球科学版), 42(增刊3):1-13.
      [42] 赵耀, 姚光庆, 穆立华, 等, 2016.塘沽地区湖相白云岩储层裂缝特征及其控制因素.地球科学, 41(2):252-264. http://www.cqvip.com/QK/94035X/201602/668415644.html
      [43] 周立宏, 卢异, 肖敦清, 等, 2011.渤海湾盆地歧口凹陷盆地结构构造及演化.天然气地球科学, 22(3):373-382. http://www.cqvip.com/QK/97226X/201103/38333540.html
      [44] 周书欣, 1992.我国湖相碳酸盐岩研究现状.石油与天然气地质, 13(4):461-462. doi: 10.11743/ogg19920413
    • 加载中
    图(9)
    计量
    • 文章访问数:  5120
    • HTML全文浏览量:  1825
    • PDF下载量:  19
    • 被引次数: 0
    出版历程
    • 收稿日期:  2017-02-11
    • 刊出日期:  2017-12-15

    目录

      /

      返回文章
      返回