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天然气地球科学 ›› 2011, Vol. 22 ›› Issue (1): 66–72.doi: 10.11764/j.issn.1672-1926.2011.01.66

• 天然气地质学 • 上一篇    下一篇

鄂尔多斯盆地镇泾地区中生界油气二次运移动力研究

丁晓琪, 张哨楠, 易超, 谢世文   

  1. 成都理工大学“油气藏地质及开发工程”国家重点实验室，四川 成都 610059
  • 收稿日期:2009-12-28 修回日期:2010-05-01 出版日期:2011-02-10 发布日期:2011-02-10
  • 通讯作者: 丁晓琪xiaoqiding@qq.com E-mail:xiaoqiding@qq.com
  • 作者简介:丁晓琪（1981-），男，甘肃武威人，博士后，主要从事储层沉积学与油藏地球化学研究.
  • 基金资助:

    国家自然科学青年基金项目“鄂尔多斯盆地晚三世延长期几个关键性事件沉积及其与油气聚集关系研究”（编号：40602012）资助

Dynamic of Mesozoic Hydrocarbon Secondary Migration in Zhenjing Oilfield, Southwestern Ordos Basin

DING Xiao-Qi, ZHANG Shao-Nan, YI Chao, XIE Shi-Wen   

  1. State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation,Chengdu University of Technology，Chengdu 610059，China
  • Received:2009-12-28 Revised:2010-05-01 Online:2011-02-10 Published:2011-02-10

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摘要：

鄂尔多斯盆地西南缘镇泾地区中生界油藏具有储层致密、丰度低、储量大的特点，已钻遇的多口高产井显示出中生界具有良好的油气勘探潜力。西南缘中生界具有多个油气成藏动力系统，不同的油气成藏动力系统具有不同的二次运移动力和通道。通过埋藏史、泥岩压实曲线及物性特征等研究，认为长8段超低渗透油藏的二次运移动力为上覆烃源岩的异常压力，通道主要为渗透层；长6段特低渗透油藏的二次运移动力主要为下伏烃源岩的异常压力，局部为浮力，通道主要为裂缝，其次为渗透层；而延安组油藏的二次运移动力为浮力，通道为裂缝、不整合面和渗透层。对油气二次运移动力和通道的研究，可以更加精细追踪油气运移指向，为鄂尔多斯盆地西南缘下一步的油气勘探提供理论依据。

关键词: 二次运移, 浮力, 异常压力, 镇泾地区, 鄂尔多斯盆地

Abstract:

The Mesozoic reservoirs in Zhenjing oilfield is characterized by tight reservoirs, low permeability, low abundance and large reserves. It has favorable exploration potential which is shown by the drilled high-yielding wells. Previous studies indicate that there are multiple dynamic systems for hydrocarbon migration and accumulation in the southwestern Ordos basin. And different systems have different dynamic and carrier path for secondary migration. Through the research on buried history, mudstone compaction curve and physical property of reservoirs, it is concluded that the dynamic of secondary migration in Chang8 Member with ultra-low permeable reservoir is overlying abnormal pressure but Yan'an reservoir is buoyancy. Besides, hydrocarbon in Chang6 Member reservoir which is characterized by low permeability accumulated through underlying abnormal pressure mainly and buoyancy locally. Furthermore, permeable bed is the chief carried path in Chang8 Member, while fracture becomes the primary path in Chang6 Member. Permeable bed is the subordinate way for Chang6 Member reserviors. As for Yan'an Formation, various channels including fracture, unconformity and permeable bed could carry hydrocarbon. From the study on dynamic and carrier path of secondary migration, tracking the hydrocarbon movement can become more accurate and exploratory theories for further exploration.

Key words: Secondary migration, Buoyancy, Abnormal pressure, Zhenjing Oilfield, Ordos basin.

中图分类号: 

  • TE122.1

［1］Bachu B.Flow systems in the Alberta basin:Pattern,types and driving mechanisms［J］.Bulletin of Canadian Petroleum Geology,1999,47(4):455-474.
［2］Pang Xiongqi,Jin Zhijun,Zuo Shengjie.Dynamics,models and classification of hydrocarbon accumulations［J］.Earth Science Frontiers,2000,7(4):507-514.［庞雄奇,金之钧,左胜杰.油气藏动力学成因模式与分类［J］.地学前缘,2000,7(4):507-514.］
［3］Tian Shichen,Cheng Yongjin,Zhang Xingguo,et al.The fluid dynamics mechanism in migration-accumulation dynamics system［J］.Earth Science Frontiers,2001,8(4):329-336.［田世澄,陈永进,张兴国,等.论成藏动力系统中的流体动力学机制［J］.地学前缘,2001,8(4):329-336.］
［4］Liu Xinshe,Xi Shengli,Huang Daojun.Dynamic conditions of Mesozoic petroleum secondary migration,Ordos basin［J］.Peroleum Exploration and Development,2008,35(2):143-147.
［5］Duan Yi,Wu Baoxiang,Zheng Chaoyang,et al.Pool-forming dynamic properties of Xifeng oilfield in Ordos basin［J］.Acta Petrolei Sinica,2005,26(4):29-34.［段毅,吴保祥,郑朝阳,等.鄂尔多斯盆地西峰油田油气成藏动力学特征［J］.石油学报,2005,26(4):29-34.］
［6］He Zixin.The Evolution and Petroleum in Ordos Basin ［M］.Beijing:Petroleum Industry Press,2003.［何自新.鄂尔多斯盆地演化与油气［M］.北京:石油工业出版社,2003.］［7］Ding Xiaoqi,Zhang Shaonan,Liu Yan.Relationship between Pre-Jurassic palaeogeomorphology and oil distribution of Zhenjing oilfield in south Ordos basin［J］.Journal of Earth Sciences and Environment,2008,30(4):385-388.［丁晓琪,张哨楠,刘岩.鄂尔多斯盆地南部镇泾油田前侏罗纪古地貌与油层分布规律［J］.地球科学与环境学报,2008,30(4):385-388.］
［8］Guo  Zhengquan,Zhang Lirong,Chu Meijuan,et al.Pre-Jurassic palaeogeomorphic control on the hydrocarbon accumulation in the lower Yanan Formation in southern Ordos basin［J］.Journal of Palaeogeography,2008,10(1):63-69.［郭正权,张立荣,楚美娟,等.鄂尔多斯盆地南部前侏罗纪古地貌对延安组下部油藏的控制作用［J］.古地理学报,2008,10(1):63-69.］
［9］Ding Xiaoqi,Zhang Shaonan,Liu Pengkun,et al.Oil reservoir distribution in sequence framework of Yanchang Formation,Zhenjing block［J］.Journal of Southwest Petroleum Univesity,2008,30(2):49-54.［丁晓琪,张哨楠,刘朋坤,等.镇泾区块延长组层序地层格架下油层富集规律［J］.西南石油大学学报，2008,30(2):49-54.］
［10］Yang Youyun,Zhang Pengbo,Zhang Zhongyi.Sedimentary features and sequence evolution of braided river delta of Chang 8 oil formation of Xifeng oil field in Ordos basin［J］.Geological Science and Technology Information,2005,24(1):45-49.［杨友运,张蓬勃,张忠义.鄂尔多斯盆地西峰油田长8油组辫状河三角洲沉积特征与层序演化［J］.地质科技情报,2005,24(1):45-49.］
［11］Zhao Wenzhi,Hu Suyun,Wang Zecheng,et al.Key role of basement fault control on oi accumulation of Yanchang Formation,upper Triassic,Ordos basin［J］.Petroleum Exploration and Development,2003,30(5):1-5.［赵文智,胡素云,汪泽成,等.鄂尔多斯盆地基底断裂在上三叠统延长组石油聚集中的控制作用［J］.石油勘探与开发,2003,30(5):1-5.］
［12］Xi Shengli,Liu Xinshe.Petroleum secondary migration pathway in Mesozoic period,Ordos basin［J］.Journal of Northwest University:Natural Science Edition,2005,35(5):628-632.［席胜利,刘新社.鄂尔多斯盆地中生界石油二次运移通道研究［J］.西北大学学报:自然科学学版,2005,35(5):628-632.］
［13］Zeng Lianbo,Gao Chunyu,Qi Jiafu,et al.Distribution and permeable of reservoir fractures,Longdong area of south Ordos basin［J］.Science in China:Series D,Earth Sciences,2008,38（supplement）:41-47.［曾联波,高春宇,漆家福,等.鄂尔多斯盆地陇东地区特低渗透砂岩储层裂缝分布规律及其渗流作用［J］.中国科学:D辑,地球科学,2008,38（增刊）:41-47.］
［14］Zeng Lianbo,Li Zhongxing,Shi Cheng′en,et al.Characteristics and origin of fractures in the extra low-permeability sandstone reservoirs of the upper Triassic Yanchang Formation in the Ordos basin［J］.Acta Geological Sinica,2007,81(2):174-180.［曾联波,李忠兴,史成恩,等.鄂尔多斯盆地上三叠统延长组特低渗透砂岩储层裂缝特征及成因［J］.地质学报,2007,81(2):174-180.］
［15］Wang Yuncheng.Oil and Gas Reservoir Evaluation［M］.Beijing:Petroleum Industry Press,1999.［王允诚.油气储层评价［M］.北京:石油工业出版社,1999.］
［16］Huang Zhilong,Jiang Qingchun,Xi Shengli,et al.Study on oil and gas accumulation period of Yanchang Formation of Triassic and Jurassic in north Shanxi slope zone,Ordos basin［J］.Journal of Xi′an Shiyou University:Natural Science Edition,2009,24(1)：21-24.［黄志龙,江青春,席胜利,等.鄂尔多斯盆地陕北斜坡带三叠系延长组和侏罗系油气成藏期研究［J］.西安石油大学学报:自然科学版,2009,24(1)：21-24.］
［17］Zhao Mengwei,Behr H J.Vitrinite reflectance in Triassic with relation to geothermal history of Ordos basin［J］.Acta Petrolei Sinica,1996,17(2):15-23.［赵孟为,Behr H J.鄂尔多斯盆地三叠系镜质体反射率与地热史［J］.石油学报,1996,17(2):15-23.］
［18］Zhao Mengwei,Behr H J,Ahrendt H.Thermal and tectonic history of the Ordos basin,China:Evidence apitite fission track analysis,vitrinite reflectance and K-Ar dating［J］.AAPG Bulletin,1996,80(7):1110-1134.
［19］Zhang Wenzheng,Yang Hua,Li Jianfeng,et al.Leading effect of high-class source rock of Chang 7 in Ordos basin on enrichment of low permeability oil-gas accumulation:Hydrocarbon generation and expulsion mechanism［J］.Petroleum Exploration and Development,2006,33(3):289-293.［张文正,杨华,李剑锋,等.论鄂尔多斯盆地长7段优质油源岩在低渗透油气成藏富集中的主导作用——强生排烃特征及机理分析［J］ 石油勘探与开发,2006,33(3):289-293.］
［20］Jansa L F,Noguera urea V H.Geology and diagenetic history of overpressured sandstone reservoir,venture gas field,offshore Nova Scotia,Canada［J］.AAPG Buuetin,1990,74(10):1640-1658.
［21］Lubanzadio M,Goulty N R,Swarbrick R E.Dependence of sonic velocity on effective stress in north sea mesozoic mudstones［J］.Marine and Petroleum Geology,2006,23(6):647-653.
［22］Hunt J M.Generation and migration of petroleum from abnormal pressured fluid compartments［J］.AAPG Buuetin,1990,74(1):1-12.
［23］Guo Xiaowen,He Sheng,Liu Keyu,et al.Oil generation as the dominant overpressure mechanism in the Cenozoic Dongying depression,Bohai Bay basin,China［J］.AAPG Buuetin,2010,94(12):1859-1881.
［24］Li Chuanliang.Downward migration of oil and gas can not occur［J］.Lithologic Reservoirs,2009,21(1):6-10.［李传亮.油气倒灌不可能发生［J］.岩性油气藏,2009,21(1):6-10.］
［25］Li Chuanliang,Zhang Jinglian,Du Zhiming.New viewpoints of the primary migration of oil and gas［J］.Earth Science Frontiers,2007,14(4):132-142.［李传亮,张景廉,杜志敏.油气初次运移理论新探［J］.地学前缘,2007,14(4):132-142.］
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