岩性油气藏 ›› 2015, Vol. 27 ›› Issue (3): 32–42.doi: 10.3969/j.issn.1673-8926.2015.03.005

• 油气地质 • 上一篇    下一篇

湖相“白烟型”喷流岩——新型的致密油储层类型—— — 以准噶尔盆地西缘乌尔禾地区风城组为例

傅 饶1,郑荣才1,常海亮1,祁利祺2,文华国1,李 云1   

  1.  1. 成都理工大学 油气藏地质及开发工程国家重点实验室,成都 610059 ;2. 中国石油新疆油田分公司 实验检测研究院,新疆 克拉玛依 834000
  • 出版日期:2015-05-26 发布日期:2015-05-26
  • 作者简介:傅饶( 1988- ),女,成都理工大学在读硕士研究生,研究方向为沉积学。 地址:( 610059 )四川省成都市成华区二仙桥东三路 1 号成都理工大学。 E-mail : 707788153@qq.com
  • 基金资助:

    高等学校博士学科点专项科研基金“准噶尔盆地西北缘二叠系湖相白云质喷流岩成因与物质组分特征研究”(编号: 20135122110004 )和国家自然科学基金面上项目“湖相白云质喷流岩物质组分对比与成因机理研究”(编号: 41472088 )联合资助

Lacustrine “ white smoke type ” exhalative rock — A new type of tight oil reservoir: A case study from Lower Permian Fengcheng Formation in Urho area, western margin of Junggar Basin

FU Rao1, ZHENG Rongcai1, CHANG Hailiang1, QI Liqi2, WEN Huaguo1, LI Yun1   

  1.  1. State Key Laboratory of Oil & Gas Reservoir Geology and Exploitation , Chengdu University of Technology , Chengdu 610059 , China ;2. Research Institute of Experiment and Detection , PetroChina Xinjiang Oilfield Company , Karamay 834000 , Xinjiang , China
  • Online:2015-05-26 Published:2015-05-26

摘要:

下二叠统风城组为准噶尔盆地西缘乌尔禾地区重要的原油产层, 储层岩性为云质岩类,具有典型的致密储层性质,为一类成因尚不为人们所熟悉的、但具备巨大油气勘探开发潜力的新型湖相“白烟型”喷流岩。 以岩心观察描述、薄片鉴定、扫描电镜观察、X射线衍射和物性分析资料为基础,以热水沉积学理论为指导,探讨了此类致密油储层的成因特征,提出同期火山喷发-湖底热液喷流-“内、外源”碎屑掺合的混合沉积模式,确定储层发育和分布受 4 种因素控制:①半深湖—深湖环境为湖底喷流岩致密油储层的发育奠定了物质基础;②构造破裂和溶蚀是改善储层物性和在致密油储层中形成“甜点”的主要作用方式; ③区域构造格局和断裂构造的继承性活动,控制了喷流岩致密油储层的区域分布,提供了同期火山喷发、热液喷流、成岩期流体溶蚀改造及油气运移成藏的通道;④半深湖—深湖相“白烟型”喷流岩聚集区中具备多期次构造破裂和热液溶蚀作用的叠合部位,是有利的致密油储层“甜点”分布位置,也是致密油藏的预测目标。

关键词: 云质岩类;&ldquo, 白烟型&rdquo, 喷流岩;新型致密油储层;下二叠统风城组;乌尔禾地区;准噶尔盆地

Abstract:

 As the representative of tight oil reservoir of Lower Permian Fengcheng Formation in Urho area, western margin of Junggar Basin, dolomitized rocks has great potential for oil and gas exploration and development of the “whitesmoke type” exhalative rock tight oil reservoir. Based on core observation and description, thin section analysis, scanning electron microscope, X ray diffraction and property analysis data, under the guidance of hot water sedimentary theory, this paper discussed the causes of these characteristics of tight oil reservoir, proposed mixed sedimentary model of volcanic eruption-sublacustrine hydrothermal jet flow—“internal and external sources”. The development and distribution of reservoir are controlled by four factors: (1)the semi deep lake-deep lake environment laid material foundation for the development of sublacustrine exhalative rock tight oil reservoir; (2)tectonic disruption and dissolution improved reservoir and the formation of “sweets” in tight oil reservoir; (3)the regional distribution of exhalative rock tight oil reservoir is controlled by regional tectonic framework and tectonic inheritance activities, provides the volcano hydrothermal fluid, diagenetic dissolution and alteration and migration of oil and gas accumulation in channel; (4)the semi-deep to deep lacustrine facies “white smoke type” exhalative rock areas with multi-phase tectonic fracture and thermal dissolution is favorable tight oil reservoir “sweets” location, but also for the prediction of target of dense reservoir.

Key words: dolomitized rocks, “white smoke type&rdquo, exhalative rock, new type of tight oil reservoir, Lower Permian , Fengcheng Formation, Urho area, Junggar Basin

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