石油与天然气地质 ›› 2015, Vol. 36 ›› Issue (2): 262-270.doi: 10.11743/ogg20150211

• 层序与储层 • 上一篇    下一篇

渤海海域蓬莱9-1花岗岩潜山大型油气田储层发育特征与主控因素

王昕1, 周心怀1, 徐国胜2, 刘朋波1, 高坤顺1, 官大勇1   

  1. 1. 中海石油(中国)有限公司 天津分公司, 天津 300452;
    2. 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:2014-01-17 修回日期:2014-12-20 出版日期:2015-04-08 发布日期:2015-05-13
  • 作者简介:王昕(1972-),男,高级工程师,石油地质.E-mail:wangxin5@cnooc.com.cn.
  • 基金资助:
    国家科技重大专项(2011ZX05023-002).

Characteristics and controlling factors of reservoirs in Penglai 9-1 large-scale oilfield in buried granite hills, Bohai Sea

Wang Xin1, Zhou Xinhuai1, Xu Guosheng2, Liu Pengbo1, Gao Kunshun1, Guan Dayong1   

  1. 1. Tianjin Branch, CNOOC, Tianjin 300452, China;
    2. State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation Engineering, Chengdu University of Technology, Chengdu, Sichuan 610059, China
  • Received:2014-01-17 Revised:2014-12-20 Online:2015-04-08 Published:2015-05-13

摘要: 蓬莱9-1油田是近年来中国近海首次发现的一个以中生代花岗岩潜山风化壳为储层的大型油气田。在花岗岩潜山这个新的勘探领域,储层特征及储层形成机理条件是制约高效勘探的关键。通过镜下薄片鉴定、扫描电镜分析、矿物X-衍射分析、岩心与岩屑录井、测井曲线等资料综合分析,认为由表及里随着风化淋滤作用的逐渐减弱,蓬莱9-1花岗岩潜山可以划分为土壤带、砂-砾质风化带、裂缝带和基岩带,储集空间由孔隙型—裂缝-孔隙型—孔隙-裂缝型—裂缝型呈现有规律的变化。花岗岩潜山储层发育主要受表生岩溶作用、有机酸溶蚀作用、构造变形作用及微古地貌作用共同控制。这个认识对中国燕山期侵入的花岗岩潜山风化壳油气勘探开发具有借鉴意义。

关键词: 风化壳, 花岗岩潜山, 燕山期, 蓬莱9-1油田, 渤海海域

Abstract: Penglai 9-1 oilfield has been the first large-scale field found in weathering crust reservoirs of the Mesozoic bu-ried granite hills in coast waters of China in recent years.In this brand new area of exploration,reservoir characterization and its forming mechanism are considered essential for efficient and successful exploration.Thin section,SEM,and clay mineral X-diffraction analyses were combined with logging data to provide insight into uncertainties of the area.The results show that the buried granite hills can be divided into soil zone,sand-conglomerate weathering zone,fracture zone and base rock zone,and reservoiring space in them changes in a regular pattern from pore to fracture-pore,pore-fracture and fracture,from the surface to the center as weathering and leaching gradually weaken.Horizontally,granite reservoirs are continuously and widely distributed and paralleled to the top of the buried hills.Thicker reservoirs are mainly developed near large-scale faults with intensive activities and paleogeomorphic slope areas.The paper proposes that the reservoirs were controlled mainly by epigenic karstification,organic acid dissolution,structural deformation and micro-palaeogeomorphology.The significance of the understanding may be felt in the future exploration and development of oil and gas in weathering curst reservoirs of buried granite hills intruded during Yanshan period.

Key words: weathering crust, buried granite hill, Yanshanian, Penglai 9-1 oilfield, Bohai Sea

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