新疆石油地质 ›› 2026, Vol. 47 ›› Issue (1): 46-56.doi: 10.7657/XJPG20260105

• 油气勘探 • 上一篇    下一篇

玛湖凹陷风城组古沉积环境特征及其对页岩油甜点的影响

陈绍蓉1(), 赵毅1, 邹阳1, 任海姣1, 陈方文2, 吴俊军1   

  1. 1.中国石油 新疆油田分公司 勘探开发研究院新疆 克拉玛依 834000
    2.中国石油大学(华东) 地球科学与技术学院山东 青岛 266580
  • 收稿日期:2025-04-30 出版日期:2026-02-01 发布日期:2026-01-23
  • 作者简介:陈绍蓉(1989-),女,重庆万州人,工程师,博士,非常规油气地质,(Tel)15801290876(Email)shaorong_chen@163.com
  • 基金资助:
    新疆维吾尔自治区“天池英才”引进计划(25XJYTSQ041);中国石油新疆油田重点研发项目(2024XJZD01)

Influences of Paleo-Sedimentary Environment on Shale Oil Sweet Spots in the Fengcheng Formation, Mahu Sag, Junggar Basin

CHEN Shaorong1(), ZHAO Yi1, ZOU Yang1, REN Haijiao1, CHEN Fangwen2, WU Junjun1   

  1. 1. Research Institute of Exploration and Development, Xinjiang Oilfield Company, PetroChina, Karamay, Xinjiang 834000, China
    2. School of Geosciences, China University of Petroleum (East China), Qingdao, Shandong 266580, China
  • Received:2025-04-30 Online:2026-02-01 Published:2026-01-23

摘要:

准噶尔盆地玛湖凹陷二叠系风城组的古沉积环境特征控制了页岩油甜点发育,但碱湖古沉积环境对页岩油甜点控制机制不清,制约了页岩油高效勘探和开发。因此,基于玛页1井风城组岩心、地球化学和测井等资料,分析了不同品质烃源岩、储集层和源-储组合形成的古水深、古气候、古盐度和古氧化还原条件,剖析了古沉积环境对页岩油甜点发育的影响。研究表明:玛页1井风城组优质Ⅰ类源-储组合形成于古水深变化相对较小、古气候相对暖湿且碳酸盐和陆源碎屑沉积物含量较高、古盐度相对较低的咸水环境和古还原条件更强的沉积环境。适宜的沉积环境为高产烃率藻类有机质絮凝和富集提供条件,促进了高初级生产力的形成,并为有机质保存提供条件,促进较低成熟度有机质大量生烃。夹层型、纹层型和纯页岩型的源-储组合分别对应Ⅰ类、Ⅱ类和Ⅲ类源-储组合,排油效率依次降低;古沉积环境通过“源-储-保”三元机制影响页岩油甜点发育。确定了风城组古沉积环境对页岩油甜点发育的控制机制,为页岩油勘探提供理论支撑。

关键词: 准噶尔盆地, 玛湖凹陷, 风城组, 古沉积环境, 页岩油, 甜点, 源-储组合

Abstract:

The paleo-sedimentary environment of the Permian Fengcheng formation in the Mahu sag of the Junggar Basin controlled the development of shale oil sweet spots. However, such controlling mechanism in alkaline lake environment is unclear, which restricts the efficient exploration and development for shale oil. Based on the core, geochemical and logging data of the Fengcheng formation in Well MY1, the paleo-sedimentary environment parameters (e.g. paleo-water depth, paleo-climate, paleo-salinity, and paleo-redox conditions) of different qualities of source rocks, reservoirs, and source-reservoir assemblages were analyzed, and the influences of paleo-sedimentary environment on the development of shale oil sweet spots were dissected. The results show that the Class Ⅰ high quality source-reservoir assemblages of the Fengcheng formation in Well MY1 were formed in the saltwater environment with a relatively small range of paleo-water depth, relatively warm and humid paleo-climate, relatively high contents of carbonate and terrigenous clastic sediments, and relatively low paleo-salinity, and also in the environment with stronger paleo-reduction condition. An appropriate sedimentary environment provides a possibility for the flocculation and enrichment of algae organic matters featuring a high hydrocarbon yield, promotes the formation of primary productivity, and contributes organic matter preservation conditions, allowing for extensive hydrocarbon generation from organic matters with relatively low maturity. The interlayered, laminar, and pure shale-type source-reservoir assemblages respectively correspond to the Class Ⅰ, Class Ⅱ and Class Ⅲ source-reservoir assemblages in a descending order of oil expulsion efficiency. It is determined that the paleo-sedimentary environment controls the development of shale oil sweet spots in the Fengcheng formation through a three-factor (source-storage-preservation) mechanism. This research insight provides a theoretical support for shale oil exploration.

Key words: Junggar Basin, Mahu sag, Fengcheng formation, paleo-sedimentary environment, shale oil, sweet spot, source-reservoir assemblage

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