中国石油勘探 ›› 2020, Vol. 25 ›› Issue (3): 134-145.DOI: 10.3969/j.issn.1672-7703.2020.03.012

• 石油地质 • 上一篇    下一篇

鄂尔多斯盆地中东部奥陶系盐下侧向供烃成藏特征及勘探潜力

包洪平1,2 ,黄正良1,2 ,武春英1,2 , 魏柳斌1,2 ,任军峰1,2 ,王前平1,2   

  1. 1 中国石油长庆油田公司勘探开发研究院;2 低渗透油气田勘探开发国家工程实验室
  • 出版日期:2020-05-15 发布日期:2020-05-15
  • 基金资助:
    国家科技重大专项“鄂尔多斯盆地奥陶系—元古界成藏条件研究与区带目标评价”(2016ZX05004-006);中国石油天然 气集团公司重大专项“鄂尔多斯盆地碳酸盐岩新领域综合研究与区带分析”(2016E-0514)。

Hydrocarbon accumulation characteristics and exploration potential of Ordovician pre-salt formations by lateral hydrocarbon supply in the central-eastern Ordos Basin

Bao Hongping1,2,Huang Zhengliang1,2, Wu Chunying1,2, Wei Liubin1,2, Ren Junfeng1,2, Wang Qianping1,2   

  1. 1 Research Institute of Exploration and Development, PetroChina Changqing Oilfield Company; 2 National Engineering Laboratory for Exploration and Development of Low Permeability Oil and Gas Fields
  • Online:2020-05-15 Published:2020-05-15
  • Supported by:
     

摘要: 鄂尔多斯盆地中东部奥陶系马家沟组发育厚达近千米的碳酸盐岩与膏盐岩共生的地层组合,埋深偏大。 这套远离风化壳的奥陶系盐下层系能否具备烃源有效供给及规模成藏,是制约勘探的关键问题。基于奥陶系沉积期后 构造演化及其与上古生界煤系烃源层配置关系的研究,认为奥陶系盐下在邻近古隆起区存在与上古生界煤系烃源层直 接接触且规模性分布的供烃窗口,窗口区在生排烃高峰期处于构造下倾部位,生烃增压等因素产生运移动力,有利于 天然气向高部位运聚;膏盐岩封盖层与白云岩储集体横向连续稳定分布构成良好的储盖组合;盆地中东部奥陶系盐下 具有规模成藏的潜力,乌审旗—靖边—延安一带为有利勘探区,值得勘探重视。

 

关键词: 供烃窗口, 侧向供烃, 奥陶系盐下, 岩性圈闭, 运移动力, 鄂尔多斯盆地

Abstract: A stratigraphic combination of carbonate rocks and gypsum rocks is developed in the Ordovician Majiagou Formation in the central-eastern Ordos Basin, with a thickness of nearly 1000 m and relatively large burial depth. The key issue restricting exploration is whether there is effective hydrocarbon supply and large-scale hydrocarbon accumulation in the Ordovician pre-salt strata, which is far away from the weathering crust. Based on research on the tectonic evolution of the Ordovician in the later sedimentary period, and the allocation relation between the Ordovician strata and the coal-bearing source rocks in the upper Paleozoic, it is considered that there is a hydrocarbon supply window for the Ordovician pre-salt strata in the areas adjacent to the paleo-uplift, which are in direct contact with the coal-bearing source rocks of the upper Paleozoic and are distributed on a large scale. The window zone was in a downdip structural position during the peak of hydrocarbon generation and expulsion. Favorable factors such as hydrocarbon generation and pressurization have provided migration force, which is conducive to the migration and accumulation of natural gas towards high positions. A good reservoir-cap assemblage is formed by continuous and stable lateral distribution of gypsum cap rocks and dolomite reservoirs. There is potential for large-scale hydrocarbon accumulation in the Ordovician pre-salt formations in the central-eastern part of the basin. The Wushenqi-Jingbian-Yan'an area is favorable for exploration and should receive more attention in the future.

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