天然气地球科学

• 天然气地质学 • 上一篇    下一篇

渤海湾盆地沧东凹陷南皮斜坡地质特征与油气成藏

周立宏,时筱淞,官全胜,杨朋,林伶,吴佳朋   

  1. 1.中国石油大港油田分公司,天津 300280;2.大港油田勘探开发研究院,天津 300280
  • 收稿日期:2016-11-10 修回日期:2017-08-27 出版日期:2017-09-10 发布日期:2017-09-10
  • 通讯作者: 时筱淞(1986-),男,吉林通化人,工程师,硕士,主要从事目标评价研究. E-mail:shixsong@petrochina.com.cn
  • 作者简介:周立宏(1968-),男,河北故城人,教授级高级工程师,博士,主要从事石油地质研究.E-mail:zhoulh@petrochina.com.cn.
  • 基金资助:

    中国石油天然气集团重大科技专项“大港油区大油气田勘探开发关键技术研究”(编号:2014E-06-03)资助.

Geological characteristics and hydrocarbon accumulation  of Nanpi Slope in the Cangdong Sag,Bohai Bay Basin

Zhou Li-hong,Shi Xiao-song,Guan Quan-sheng,Yang Peng,Lin Ling,Wu Jia-peng   

  1. (1.PetroChina Dagang Oilfield Company,Tianjin 300280,China; 
    2.Exploration and Development Research Institute of Dagang Oilfield Company,PetroChina,Tianjin 300280,China
  • Received:2016-11-10 Revised:2017-08-27 Online:2017-09-10 Published:2017-09-10

摘要:

随着沧东凹陷正向构造带油气藏勘探程度的不断提高,成藏区带规模发现遇到瓶颈,勘探思路必须由构造油气藏勘探向斜坡连续性油气藏勘探转变。通过对沧东凹陷南皮斜坡精细构造解释、沉积微相划分、烃源岩特征及区域控砂控藏机制的分析,获得南皮斜坡地质特征与油气成藏模式的认识。研究表明,南皮斜坡为宽缓继承性斜坡,构造呈现高、中、低斜坡三分性特点,古近系孔店组二段(孔二段Ek2)发育辫状河三角洲沉积,孔店组一段(孔一段Ek1)底部发育浅水三角洲、上部发育冲积扇沉积,有利砂体大面积发育,孔二段发育好—很好烃源岩,生烃强度大。以构造、砂体、烃源岩及已知油藏匹配,形成自源成藏、它源成藏两大成藏组合系统,并构建孔二段有效生油岩范围内,中斜坡孔二段主砂体区常规油藏聚集,低斜坡远端细粒沉积岩类与油页岩叠合形成致密油,含油气系统范围内常规油与致密油叠加连片,形成“连续性成藏”油气成藏模式;孔一段受孔二段有效烃源岩控制下,形成“底部砂组近源大面积充注、上部继承性断裂网状沟通”的复合聚油模式。

关键词: 南皮斜坡, 构造油藏, 自源成藏, 连续性成藏

Abstract:

With increasing exploration degree of hydrocarbon reservoirs in the forward structural belt,the large-scale discovery of Tibet entered a bottleneck.The exploration idea must change from structural reservoir exploration to slope continuous reservoir exploration.By analyzing fine structure interpretation,sedimentary microfacies division,source rock characteristics and regional sand control mechanism of Nanpi Slope in the Cangdong Sag,we get the understanding of the geological features of the Nanpi Slope and the model of oil and gas accumulation.The study shows that the Nanpi Slope is a broad and gentle inherited slope,and the structure shows three characteristics of high,medium and low slopes.The Ek2 formation develops Braided River Delta in Paleogene,shallow delta is developed at the bottom of Ek1 formation,and alluvial fan sedimentary environment is developed in the upper part.The environment development is favorable for large areas of sand bodies.High quality source rocks developed in the  Ek2  formation,with high hydrocarbon generating intensity.Based on the matching of structure,sand body,source rock and known reservoir,two reservoir forming combination systems of self\|source accumulation and other source accumulation are formed.In the effective oil source rock range,the conventional reservoir accumulated in the middle slope main sand body area,the low slope and the distal fine-grained sedimentary rock overlap with oil shale to form tight oil in Ek2 .In oil and gas system,conventional oil and tight oil overlap to form a model of continuous accumulation.Under the control of Ek2 effective hydrocarbon source rocks,Ek1 formed a composite oil accumulation model of “bottom sand group,near source,large area filling,upper succession fault and network communication”.

Key words: Nanpi Slope, Structural reservoir, Self-source accumulation, Continuous accumulation

中图分类号: 

  • TE122.2

[1]Zhao Limin,Zhao Xianzheng,Liu Jingwang,et al.Characteristics of Paleogene stratigraphic and lithologic reservoirs and its exploration direction in Jizhong Depression[J].Acta Petrolei Sinica.2009,30(4):492-497.[赵力民,赵贤正,刘井旺,等.冀中坳陷古近系地层岩性油藏成藏特征及勘探方向[J].石油学报.2009,30(4):492-497.]
[2]Li Hongxiang,Gao Yong,Li Huishen et al.Hydirocarbon accumulation and distributed model of lithologic reservoir in the slope of Qikou Sag[J].Natural Gas Geoscience,2010,21(4):581-583.[李洪香,高勇,李会慎,等.歧口凹陷斜坡区油气运聚特征及岩性油气藏分布模式[J].天然气地球科学,2010,21(4):581-583.]
[3]Li Hongjun,Li Huishen,Zeng Jianhong,et al.Kong 2 member hydrocarbon and controlling factors in Nanpi Slope[J].Special Oil and Gas Reservoirs,2015,22(1):57-59.[李宏军,李会慎,曾建宏,等.南皮斜坡孔二段油气分布规律及主控因素分析[J].特种油气藏,2015,22(1):57-59.]
[4]Xu Zuxin,Zhang Yijie,Wang Jufeng,et al.Relationship between conventional oil and tight oil in the second member of Kongdian Formation,Cangdong Sag[J].Journal of China University of Mining & Technology,2016,45(2):330-331.[徐祖新,张义杰,王居峰,等.沧东凹陷孔二段常规油与致密油关系研究[J].中国矿业大学学报,2016,45(2):330-331.]
[5]Wang Zhensheng,Guan Quansheng,Tan Zhenhua,et al.Study on depositional system characteristics of Ek1 in Cangdong Depression[J].Petroleum Geology and Engineering,2016,30(6):56-57.[王振升,官全胜,谭振华,等.沧东凹陷孔一段沉积体系特征研究[J].石油地质与工程,2016,30(6):56-57.]
[6]Li Yong,Yan Zhaokun,Li Hongxiang,et al.Paleogeography method of fault depression superposition lake basin: A case study of Cangdong Sag[J].Acta Petrolei Sinica.2016,37(S2):42-47.[李勇,颜照坤,李洪香,等.断坳叠置湖盆岩相古地理研究方法[J].石油学报,2016,37(S2):42-47.]
[7]Liu Zicang,Zhou Yuwen,Xiao Yuyong,et al.New knows about stratum deposition research in Cangdong-Nanpi Sag[J].Xinjiang Geology,2009,27(4):387.[刘子藏,周育文,肖玉永,等.沧东—南皮凹陷地层沉积研究新认识[J].新疆地质,2009,27(4):387.]
[8]Zhou Lihong,Pu Xiugang,Han Wenzhong,et al.Sedimentary characteristics and hydrocarbon exploration of Ek2 of Nanpi Slope area,Cangdong Sag,Huanghua Depression,North China[J].Journal of Chengdu University of Technology:Science & Technology Edition,2015,42(5):542-544.[周立宏,蒲秀刚,韩文中,等.沧东凹陷南皮斜坡孔二段沉积特征与油气勘探[J].成都理工大学学报:自然科学版,2015,42(5):542-544.]
[9]Xu Zuxin,Jiang Wenya,Zhang Yijie,et al.Hydrocarbon forming environment of source rocks of the second member of Kongdian Formation in Cangdong Sag,Baohai Bay Basin[J].Journal of Northeast Petroleum University,2015,39(4):73-76.[徐祖新,姜文亚,张义杰,等.渤海湾盆地沧东凹陷孔二段优质烃源岩成烃环境[J].东北石油大学学报,2015,39(4):73-76.]
[10]Liu Xiaoping,Liu Qingxin,Liu Jie,et al.Geochemical characteristics of organic-rich shales of the second member of Kongdian Formation in Cangdong Sag,Huanghua Depression[J].Lithologic Reservoirs,2015,27(6):17-20.[刘小平,刘庆新,刘杰,等.黄骅坳陷沧东凹陷孔二段富有机质泥页岩地球化学特征[J].岩性油气藏,2015,27(6):17-20.]
[11]Cao Tao,Yang Hua,Wang Zhensheng,et al.Application of the integrated exploration mode in lithologic reservoirs of Nanpi Slope[J].Mud Logging Engineering,2013,24(4):65-69.[曹涛,杨桦,王振升,等.一体化勘探模式在南皮斜坡岩性油气藏中的应用[J].录井工程,2013,24(4):65-69.]
[12]Jia Beibei,Chen Shiyue,Yan Jihua,et al.Characterization of fine-grained sedimentary microfacies in the second member of Kongdian Formation,Cangdong Sag[J].Henan Science,2016,34(3):373-374.[贾贝贝,陈世悦,鄢继华,等.沧东凹陷孔二段细粒沉积岩沉积微相研究[J].河南科学,2016,34(3):373-374.]
[13]Zhang Shun,Chen Shiyue,Pu Xiugang,et al.Lithofacies types and reservoir characteristics of fine-grained sedimentary rocks in Paleogene,southern Bohai fault-depressed lacustrine basin[J].Journal of China University of Mining &Technology,2016,45(3):569-578.[张顺,陈世悦,蒲秀刚,等.断陷湖盆细粒沉积岩岩相类型及储层特征[J].中国矿业大学学报,2016,45(3):569-578.]
[14]Chen Shiyue,Gong Wenlei,Zhang Shun,et al.Fracture characteristics and main controlling factors of shales of the second member of Kongdian Formation in Cangdong Sag,Huanghua Depression[J].Geoscience,2016,30(1):146-153.[陈世悦,龚文磊,张顺,等.黄骅坳陷沧东凹陷孔二段泥页岩裂缝发育特征及主控因素分析[J].现代地质,2016,30(1):146-153.]
[15]Zhang Yue,Chen Shiyue,Meng Qingai,et al.The discovery of analcite in fine-grained sedimentary rocks of the second member of Kongdian Formation in Cangdong Sag,Huanghua Depression:Impalications for early digenetic environment[J].China Petroleum Exploration,2015,20(4):40-42.[张跃,陈世悦,孟庆爱,等.黄骅坳陷沧东凹陷孔二段细粒沉积中方沸石的发现及其地质意义[J].中国石油勘探,2015,20(4):40-42.]
[16]Ge Wei,Li Yunpeng,Dong Xiaowei,et al.Study on hydrocarbon accumulation conditions and enrichment models of Paleogene in the eastern sag[J].Mud Logging Engineering,2012,23(3):91-92.[葛维,李云鹏,董晓伟,等.沧东凹陷古近系油气成藏条件与富集模式研究[J].录井工程,2012,23(3):91-92.]
[17]Xu Zuxin,Jiang Wenya,Chen Feiran,et al.Study on distribution and main control factor of hydrocarbon in Kong 2 member,Cangdong Sag[J].Special Oil and Gas Reservoirs,2015,22(6):15-18.[徐祖新,姜文亚,陈斐然,等.沧东凹陷孔二段油气分布序列与主控因素研究[J].特种油气藏,2015,22(6):15-18.]
[18]Li Ling,Liu Zicang,Guan Quansheng,et al.Formation conditions and exploration potential of tight oil in Kong 2 member,Cangdong Sag [J].Petroleum Geology and Engineering,2015,29(6):8-9.[林伶,刘子藏,官全胜,等.沧东凹陷孔二段致密油形成条件与勘探潜力[J].石油地质与工程,2015,29(6):8-9.]
[19]Liu Guoquan,Jia Li.Forming conditions and potential of tight oil in Cangdong Sag[J].Special Oil and Gas Reservoirs,2014,21(5):58.[刘国全,贾丽.沧东凹陷致密油形成条件及勘探潜力[J].特种油气藏,2014,21(5):58.]
[20]Ma Hong,Liu Zicang,Li Hongxiang,et al.Hydrocarbon accumulation model and enrichment rules for the second member of Kongdian Formation in Nanpi Slope[J].Mud Logging Engineering,2016,27(3):75-78.[马红,刘子藏,李洪香,等.南皮斜坡孔二段成藏模式与富集规律[J].录井工程,2016,27(3):75-78.]

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