›› 2014, Vol. 35 ›› Issue (4): 1-1.

• 论文 •    

苏德尔特油田浅变质岩潜山油藏裂缝系统研究

苏向光1a,孙萌萌1b,张荻楠1a ,贾爱婷2   

  1. (1.中国石油 大庆油田有限责任公司 a. 勘探开发研究院,黑龙江 大庆 163712;b. 第三采油厂,黑龙江 大庆 163113;2.中国石油 新疆油田分公司 采油二厂,新疆 克拉玛依 834000)
  • 出版日期:2019-01-01 发布日期:1905-07-13

Study on the Fracture Systems of Epimetamorphic Rock Buried Hill Reservoir in Sudeerte Oilfield, Beier Sag in Hailar Basin

SU Xiangguang1a, SUN Mengmeng1b, ZHANG Dinan1a, JIA Aiting2   

  1. (1.PetroChina Daqing Oilfield Company Ltd., a.Research Institute of Exploration and Development, Daqing, Heilongjiang 163712, China,b.No.3 Oil Production Plant, Daqing, Heilongjiang 163113, China; 2.No.2 Production Plant, Xinjiang Oilfield Company, PetroChina, Karamay, Xinjiang 834000, China)
  • Online:2019-01-01 Published:1905-07-13

摘要: 对苏德尔特油田布达特群浅变质岩潜山油藏裂缝控制因素、潜山储集层储集类型及裂缝系统深入研究后认为,潜山储集层裂缝的形成主要与所经历的构造运动有关,具有多期形成、多期充填的特点,储集类型主要包括孔隙-缝洞型和孔隙-裂缝型两种。由于断层活动强度的差异,导致不同断块裂缝发育程度不同,活动强度大的断层附近储集层最为发育,储集层物性好,反之,储集层较不发育,物性也较差。潜山储集层裂缝发育较差的断块,纵向上存在顶部和内幕两个裂缝网络系统,两个裂缝网络系统在储集类型、储集层物性和产油能力方面存在较大差异。

Abstract: This paper presents in?depth research of the fracture?controlled factors, reservoir types and fracture systems of the epimetamorphic rock buried hill reservoir of Budate group in Sudeerte Oilfield in Hailar basin. The results show that the formation of the buried hill reservoir fractures is related to the tectonic movements here, with multistage shaping and filling features. The reservoir types mainly include the pore?fracturevug type and the pore?fracture type. The fault activity differences lead to different development of fractures in different fault blocks: near the intense faults, the reservoir rock developes best, with good petrophysical properties; while away from the faults,the reservoir rock less developes, and the petrophysical property is poor. For the fault blocks with poor developing fractures in the buried hill reservoirs, there exist top and inside fracture network systems in the vertical, which have big differences in reservoir type, petrophysical property and oil productivity, etc

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