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伏尔加—乌拉尔典型前陆盆地石油地质特征及勘探前景分析

李斌 朱筱敏

李斌, 朱筱敏. 伏尔加—乌拉尔典型前陆盆地石油地质特征及勘探前景分析[J]. 石油实验地质, 2012, 34(1): 47-52. doi: 10.11781/sysydz201201047
引用本文: 李斌, 朱筱敏. 伏尔加—乌拉尔典型前陆盆地石油地质特征及勘探前景分析[J]. 石油实验地质, 2012, 34(1): 47-52. doi: 10.11781/sysydz201201047
Li Bin, Zhu Xiaomin. Petroleum geology and exploration potential of Volga-Ural Basin:one typical foreland[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2012, 34(1): 47-52. doi: 10.11781/sysydz201201047
Citation: Li Bin, Zhu Xiaomin. Petroleum geology and exploration potential of Volga-Ural Basin:one typical foreland[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2012, 34(1): 47-52. doi: 10.11781/sysydz201201047

伏尔加—乌拉尔典型前陆盆地石油地质特征及勘探前景分析

doi: 10.11781/sysydz201201047
基金项目: 中石油基金项目“全球剩余油气资源研究及油气资源快速评价技术”(2008ZX05028-003)资助
详细信息
    作者简介:

    李斌(1970- ),男,博士后.从事沉积学及空间数据库研究.E-mail:libin9600@sohu.com.

  • 中图分类号: P618.13

Petroleum geology and exploration potential of Volga-Ural Basin:one typical foreland

  • 摘要: 伏尔加—乌拉尔盆地为东欧地台东部边缘一个典型的前陆盆地,发育前寒武里菲纪—新生代第四纪地层,其中上古生界海相碳酸盐岩地层中发育良好的生、储、盖组合,形成了巨型富油气区,具有广阔的油气资源前景。其构造演化经历了陆内裂谷碎屑岩阶段、被动陆缘碳酸盐岩台地阶段、造山带前陆盆地形成阶段以及前陆盆地碎屑岩阶段。研究表明,该盆地经历了大陆开裂—大陆碰撞整个"威尔逊旋回"的构造运动,具有典型的大型前陆盆地形成与演化特征;被动陆缘阶段发育的生物碳酸盐岩为烃源岩提供了物质基础,而在前陆盆地形成时造山带强烈的区域构造运动为油气运移提供了动力,使油气大规模聚集;盆地东部褶皱带为今后重要的勘探区。

     

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出版历程
  • 收稿日期:  2011-03-28
  • 修回日期:  2011-12-13
  • 刊出日期:  2012-01-28

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