新疆博格达山周缘构造变形特征及演化过程: 来自隐伏山体构造解析的证据

    Structural deformation characteristics and evolution process in the periphery of Bogda Mountain in Xinjiang: Evidence from structure analysis of buried mountain massifs

    • 摘要: 新疆博格达山周缘是我国重要的油气资源调查区,其构造变形及演化过程复杂,后期改造强烈,早期构造特征难以恢复,制约了油气资源调查进程。基于博格达山周缘二维地震资料的精细构造解析,聚焦隐伏的三葛庄次凸,创新性采用“隐伏山体构造解析”研究思路,系统厘定博格达山周缘的构造变形样式与演化过程。研究取得以下成果: 一是证实了三葛庄次凸为博格达山弧形造山带的隐伏端,其新生代改造弱,早期构造保存较好,为恢复博格达山构造演化提供了关键“窗口”; 二是在地震资料中识别出石炭纪—早二叠世正断层,为博格达地区裂谷盆地背景提供了关键地震学证据; 三是揭示了区域浅层构造变形以逆冲推覆为主,滑脱构造为次生,深化了对“裂谷反转”型造山带变形机制的认识。在应用层面,研究成果明确了博格达山周缘经历了3个演化阶段: 石炭纪—早二叠世裂谷盆地伸展阶段、晚二叠世—白垩纪多期次挤压造山阶段和古近纪以来差异陆内造山阶段,其中初始隆升发生在晚二叠世,大规模隆升发生在侏罗纪末—白垩纪。这一构造演化时序的厘定,为区内烃源岩分布预测、储层评价及油气勘探部署提供了重要的地质依据。

       

      Abstract: The periphery of Bogda Mountain in Xinjiang is an important oil and gas resource investigation area in China. The structural deformation and evolutionary history of this area are complex, and the tectonic reworking in late-stage was intense, making it difficult to restore early structural characteristics and constraining the progress of oil and gas exploration. Based on detailed structural analysis of 2D seismic data from the periphery of Bogda Mountain, the authors in this study focused on the newly identified Sangezhuang sub-convex and adopted a "buried mountain massif structural analysis" approach to systematically determine the structural deformation styles and evolutionary history of Bogda Mountain periphery. The theoretical contributions of this study are threefold. Firstly, it confirms that Sangezhuang sub-convex was the buried terminal of Bogda Mountain arcuate orogenic belt, and its Cenozoic tectonic modification was weak, leading to good preservation of early structures, which provided a critical "window" for restoring the tectonic evolution of Bogda Mountain. Secondly, it identifies the Carboniferous-Early Permian normal faults in the seismic data, providing key seismic evidence for a rift basin setting in Bogda region. Thirdly, it reveals that shallow structural deformation in the area is dominated by thrust nappe structures, with decollement structures being secondary, deepening the understanding of the deformation mechanisms of the "rift-inverted" orogenic belt. In terms of application, the results defined three tectonic evolution stages around Bogda Mountain, that is the Carboniferous-Early Permian rift basin extension, the Late Permian-Cretaceous multi-phase compressional orogeny, and the Paleogene-recent differential intracontinental orogeny. Among these, initial uplift occurred in the Late Permian, and large-scale uplift took place during the latest Jurassic-Cretaceous. This tectonic evolution sequence could provide crucial geological basis for predicting source rock distribution, reservoir evaluation, and oil and gas exploration deployment in this region.

       

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