伏尔加—乌拉尔盆地前中生代原型盆地演化与岩相古地理特征

作    者:冯佳睿1,温志新1,贺正军1,陈 轩2,孟庆洋1,马 超1,苏 玲1,汪永华1
单    位:1 中国石油勘探开发研究院;2 长江大学
基金项目:
摘    要:
伏尔加—乌拉尔盆地是东欧地台东缘的典型前陆盆地,常规、非常规油气储量全球占比高,但成盆成储认识 程度低。通过系统调研区域地质资料,基于前中生代不同地质时期的沉积充填特征,对盆地整体演化特征及岩相古 地理格局展开综合分析。结果表明:①伏尔加—乌拉尔盆地经历了伸展拉张、挤压碰撞构造演化阶段,发育陆内裂 谷、被动大陆边缘、弧后坳陷、弧后前陆4个原型盆地类型/阶段。②在不同原型盆地演化过程中,盆地经历了陆相— 海相—陆相的多旋回变化:中—新元古代盆地东部发生沉积作用,以陆相碎屑岩为主;早奥陶世乌拉尔洋开启,东欧 地台发生海侵,以浅海碳酸盐岩发育为主;泥盆纪开始,盆地经历多期海退与海侵交替作用;二叠纪末盆地整体抬升, 遭受剥蚀。③盆地发育 4套成藏组合,多玛尼克相烃源岩为主要烃源岩,海侵阶段的海陆过渡相和滨浅海相为盆内 两套重要的油气储层,穆哈诺沃—埃罗霍夫凹陷和喀山—上卡马坳陷分别为未来非常规和常规油气勘探重点关注的 领域。研究成果为海外油气新项目评价和勘探开发实践提供依据。
关键词:原型盆地;岩相古地理;前陆盆地;成藏组合;伏尔加—乌拉尔盆地

Evolution and lithofacies paleogeographic characteristics of the Pre-Mesozoic prototype basin in Volga-Urals Basin

Author's Name: FENG Jiarui1, WEN Zhixin1, HE Zhengjun1, CHEN Xuan2, MENG Qingyang1, MA Chao1, SU Ling1, WANG Yonghua1
Institution: 1. Research Institute of Petroleum Exploration & Development, PetroChina; 2. Yangtze University
Abstract:
The Volga-Urals Basin is a typical foreland basin on the Eastern European Platform, accounting for a significant proportion of global conventional and unconventional oil and gas reserves. However, the understanding of its basin formation and reservoir accumulation remains limited. Through systematic investigation of geological data, the evolution of the basin and its lithofacies paleogeographic characteristics are comprehensively analyzed based on the sedimentary filling features during different Pre-Mesozoic geological periods. The results show that: (1) Under the influence of different tectonic stresses such as tensional stress and compressional stress, the Volga Ural Basin underwent tectonic evolutionary stages of extensional and compressional regimes, developing four prototype basin types/stages: intracontinental rift, passive continental margin, back-arc depression, and back-arc foreland basin. (2) During different tectonic evolution processes, the basin has undergone multiple-cycle changes from terrestrial to marine and back to terrestrial. During the Meso-Neoproterozoic, the basin remained generally stable with sedimentation confined to its eastern region, dominated by terrestrial clastic deposits; in the Early Ordovician, the opening of the Ural Ocean led to a marine transgression across the East European Platform, characterized primarily by shallow marine carbonates; beginning in the Devonian, the basin underwent multiple regressive-transgressive cycles; by the end of the Permian, the entire basin was fully uplifted and subjected to erosion. (3) The basin developed four petroleum systems, with the Domanik Formation serving as the primary source rock. The transitional facies and shallow marine facies developed during the transgressive phase constitute two critical hydrocarbon reservoir units in the basin. Muhanovo-Erohovsk Sag and Kashan-Kama Depression are respectively the key area for unconventional and conventional oil and gas exploration in the future. The research findings provide a critical foundation for the evaluation of overseas oil and gas projects and the implementation of exploration and development practices.
Keywords: prototype basin; lithofacies paleogeography; foreland basin; petroleum systems; Volga-Urals Basin
投稿时间: 2025-06-30  
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