中国石油勘探 ›› 2020, Vol. 25 ›› Issue (4): 125-132.DOI: 10.3969/j.issn.1672-7703.2020.04.013

• 石油地质 • 上一篇    下一篇

滨里海盆地东缘盐下油气成藏特征与主控因素

梁爽1 ,吴亚东2 ,王燕琨1 ,王震1 ,盛善波3   

  1. 1 中国石油勘探开发研究院;2 中国石油国际勘探开发有限公司;3 中油国际阿克纠宾公司
  • 出版日期:2020-07-14 发布日期:2020-07-14
  • 基金资助:
    国家科技重大专项“全球油气资源评价与选区选带研究”(2016ZX05029);中国石油天然气集团有限公司科技管理部项目 “海外重点战略大区勘探技术与应用”(2019D-4307)。

Characteristics and principal controlling factors of sub-salt oil and gas accumulation in the eastern margin of the Precaspian Basin

Liang Shuang1, Wu Yadong2, Wang Yankun1, Wang Zhen1, Sheng Shanbo3   

  1. 1 PetroChina Research Institute of Petroleum Exploration & Development; 2 China National Oil and Gas Exploration and Development Corporation Ltd.; 3 CNPC International Aktobe Company
  • Online:2020-07-14 Published:2020-07-14
  • Supported by:
     

摘要: 滨里海盆地盐下油气资源十分丰富,是世界重要的油气产地。盆地东缘受古隆起和乌拉尔造山运动双重 影响,油气成藏控制因素复杂。通过分析油气成藏要素特点和成藏模式,提出油气成藏主控因素。盆地东缘油气成藏 与乌拉尔洋俯冲—消减—关闭的过程密切相关,这一过程产生的古裂谷、古隆起控制了油气藏的形成。古裂谷控制生 烃中心,裂谷作用产生的断裂成为油气运移主通道;古隆起控制早期碳酸盐台地形成及其上优质储层发育,同时也是 油气聚集的重要指向区;乌拉尔造山运动控制后期碳酸盐台地形成,乌拉尔造山带及其他海西期造山带使盆地演化为 封闭海环境,形成全盆地分布的空谷阶盐岩优质盖层,碰撞造山过程产生的断裂形成断层相关圈闭、改善储层性能及 导致油气二次成藏。

 

关键词: 滨里海盆地, 东缘, 乌拉尔, 盐下, 控制因素, 油气成藏

Abstract: The Precaspian Basin, which is rich in sub-salt petroleum resources, is a globally important oil and gas producing area. The controlling factors of hydrocarbon accumulation in the eastern margin of the basin are complex, where it has been affected by paleo-uplift and by the Uralian orogeny. In this paper, the principal controlling factors of oil and gas accumulation in the eastern margin of the basin are identified according to analysis of hydrocarbon accumulation factors and accumulation models. Hydrocarbon accumulation in the eastern margin of the basin is closely related to the processes of subduction, subtraction, and closure of the Ural ocean. These processes formed paleo-rifts and paleo-uplifts which controlled the formation of oil and gas reservoirs. Paleo-rifts controlled the hydrocarbon generation centers. Faults formed by rifting became the primary pathways for oil and gas migration. Paleo-uplifts controlled the formation of early carbonate platform and the development of high-quality reservoirs, which are also important directional areas for oil and gas accumulation. The Uralian orogeny controlled the formation of later carbonate platform. The Uralian and other Hercynian orogenic belts created the conditions for the evolution of the basin into a restricted marine environment, forming high-quality salt caprocks in the Kungurian stage which are distributed across the whole basin. Faults generated during the collision orogeny formed fault-related traps, improved reservoir performance, and led to secondary hydrocarbon accumulation.

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