高级检索

    鄂尔多斯盆地多种能源资源形成演化、共存特征与开采地质保障

    Coexistence characteristics of multiple energy resources and geological support for loss-reducing mining in the Ordos Basin

    • 摘要:
      研究目的 鄂尔多斯盆地是我国重要的多种能源资源富集区,呈现出“共生一盆、垂向叠置”的鲜明特征,且区内各类能源资源成因关联紧密、空间分布有序。随着大规模、高强度的资源开发进行,其与区域脆弱的生态环境之间的矛盾日益凸显。因此,立足系统科学理念,从盆地动态演化的视角出发,揭示多种能源资源的成藏(矿)规律与空间配置关系,构建开发过程中的减损地质保障路径,是实现鄂尔多斯盆地能源资源协调开发与生态保护协同推进的重要途径。
      研究方法 本文系统收集了鄂尔多斯盆地演化与能源资源赋存规律等相关的数据资料和文献,划分了盆地成藏(矿)阶段,并提出了多种能源资源协调开采地质保障思路。
      研究结果 鄂尔多斯盆地经历了中—新元古代裂陷盆地、早古生代克拉通边缘坳陷、晚古生代克拉通内坳陷及中生代残余克拉通盆地等多阶段构造演化,形成了煤、油、气、铀、氦气、地热以及铝土矿、岩盐等多能源资源共存的资源赋存框架;成藏(矿)过程与盆地演化密切关联,可划分为前寒武纪变质—岩浆成矿、早古生代沉积成矿(岩矿)、晚古生代沉积成矿(有机能源)、中生代多能源共生及新生代调整—再就位等阶段,塑造了以奥陶系、石炭—二叠系、三叠—侏罗系和白垩系四大层系为核心的多种能源资源垂向叠置结构;在时空分布上表现出明显的规律性与立体叠置特征。实现多能源资源的安全、绿色与协调开发,亟待构建以盆地演化历史与资源分布规律为核心的“多资源时空协同开发”理论框架与规划方法,并建立多圈层耦合响应的韧性减损地质保障体系。
      结论 本研究可为推动鄂尔多斯盆地能源资源的综合开发与生态保护提供科学依据,对保障国家能源安全有重要的指导意义。

       

      Abstract:
      This paper is the result of mineral exploration engineering.
      Objective The Ordos Basin is a key enrichment area for multiple energy resources in China, featuring "coexistence in a single basin and vertical superimposition" with orderly spatial distribution. With the intensification of large-scale, high-intensity resource exploitation, the conflict with the region’s fragile ecological environment has become increasingly prominent. Thus, based on systematic science and from the perspective of dynamic basin evolution, revealing the metallogenic (hydrocarbon accumulation) laws and spatial allocation of multiple energy resources, and constructing geological guarantee paths for loss reduction during exploitation are crucial to realizing coordinated energy development and synergistic ecological protection in the basin.
      Methods Relevant data and literature on basin evolution, resources, and mineral occurrence were systematically collected, summarized, and analyzed. The metallogenic (hydrocarbon accumulation) stages were divided, and geological guarantee ideas for coordinated exploitation of multiple energy resources were proposed.
      Results The basin has experienced multi-stage tectonic evolution, forming a resource framework with coexisting coal, oil, natural gas, uranium, helium, geothermal energy, bauxite, and rock salt. The metallogenic (hydrocarbon accumulation) process is closely linked to basin evolution, divided into Precambrian metamorphic-magmatic, Early Paleozoic sedimentary diagenetic (metallogenic), Late Paleozoic sedimentary metallogenic (organic energy), Mesozoic multi-energy symbiosis, and Cenozoic adjustment-repositioning stages. These stages have shaped a vertical superimposed energy structure centered on four major strata: Ordovician, Carboniferous-Permian (C-P), Triassic-Jurassic (T-J), and Cretaceous. Energy resources show distinct temporal-spatial regularity and three-dimensional superimposition, with C-P and T-J strata as key enrichment horizons. To achieve safe, green, and coordinated exploitation, it is urgent to construct a "temporal-spatial coordinated exploitation of multiple resources" theoretical framework and planning method (centered on basin evolution and resource distribution) and establish a resilient loss reduction geological guarantee system with multi-sphere coupling response.
      Conclusions This study provides a scientific basis for comprehensive energy development and ecological protection in the Ordos Basin, and has important guiding significance for safeguarding national energy security.

       

    /

    返回文章
    返回