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    中上扬子地区南华系大塘坡组沉积期岩相古地理及对油气成藏的指示

    Lithofacies paleogeography during the depositional period of the Nanhua System Datangpo Formation and its indications for hydrocarbon accumulation in the Middle and Upper Yangtze Region, South China

    • 摘要:
      研究目的 中上扬子地区在新元古代南华纪中期发育大塘坡组海相黑色含锰碳质页岩,长期以来作为锰矿层被广泛关注,但对其油气地质特征研究较少。本文从油气地质角度详细阐述了大塘坡组岩相古地理及其对油气成藏的指示作用,以期为中国南方地区油气调查提供指导。
      研究方法 通过野外地质调查和资料收集,采用单井分析、连井对比、岩相古地理图编制等方法,结合烃源岩特征分析、储层分析等实验测试手段,详细梳理了大塘坡组沉积特征和油气地质条件,分析了烃源岩特征和潜在油气组合。
      研究结果 大塘坡组形成于间冰期,沉积过程受拉张裂陷活动控制,可划分出2大类沉积相、7类沉积亚相及若干沉积微相,整个沉积期构成一个完整的海侵—高位—海退沉积旋回;大塘坡组最具油气资源潜力的相带为局限陆棚亚相和潟湖亚相,主要分布在大塘坡组一段,有机地球化学指标特征好,为优质烃源岩。
      结论 大塘坡组一段具有良好的生烃潜力和页岩气发育潜力,松桃、花垣、秀山、湘潭、鹤峰等地区具有页岩气发育有利条件,为潜在页岩气发育区。以大塘坡组为烃源岩发育多类油气成藏组合,渝黔湘交界的秀山、松桃、花垣地区源储配置条件较好,为潜在常规油气发育区。

       

      Abstract:
      This paper is the result of oil and gas exploration engineering.
      Objective The marine black manganese−bearing carbonaceous shale of the Datangpo Formation, widely distributed in the mid−Neoproterozoic Nanhua strata of the Middle−Upper Yangtze Region, South China, has been extensively studied as a manganese deposit but remains poorly investigated regarding its petroleum geological characteristics. This study systematically analyzes the lithofacies paleogeography of the Datangpo Formation and evaluates its implications for hydrocaron accumulation, providing critical insights for guiding petroleum exploration in the southern China.
      Methods Through field surveys and comprehensive data synthesis of the Datangpo Formation, we systematically evaluated hydrocarbon conditions, source rock geochemistry, and reservoir−caprock assemblage, especially lithofacies and paleogeography. This integrated approach combined individual well log interpretation, multi−well correlation analysis, and lithofacies paleogeographic with advanced analytical techniques including organic geochemical testing, petrophysical characterization, and reservoir evaluation.
      Results The Datangpo Formation developed during an interglacial period, with its depositional architecture constrained by extensional riftdynamics. Sedimentary facies within the formationare classified into two principal types, seven subcategories and multiple microfacies. The sequence comprises a complete transgressive−highstand−regressive cycle. Hydrocarbon−prospective facies are limited shelf subfacies and lagoon subfacies, predominantly occurring in the first member. These intervals exhibitfavorableorganic geochemical index, and constitute potential source rock horizons.
      Conclusions The first member of the Datangpo Formation exhibits significant hydrocarbon−generation potential and viable shale gas prospects. Strategic areas including Songtao, Huayuan, Xiushan, Xiangtan and Hefeng, located at the confluence of Hunan, Chongqing and Guizhou Province, demonstrate favorable geological conditions for shale gas exploitation. This unit serves as a competent source rock capable of forming multiple prospective hydrocarbon reservoir assemblages. Notably, The Xiushan−Songtao−Huayuan sector along the tri−province boundary of Chongqing, Guizhou, and Hunan exhibits optimal source−reservoir coupling configuration, indicating promising targets for conventional petroleum exploration.

       

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