吉林大学学报(地球科学版) ›› 2020, Vol. 50 ›› Issue (6): 1628-1638.doi: 10.13278/j.cnki.jjuese.20190082
• 地质与资源 • 上一篇
李一赫1, 王殿举2,3, 于法浩4, 刘志强5
Li Yihe1, Wang Dianju2,3, Yu Fahao4, Liu Zhiqiang5
摘要: 下刚果盆地具有巨大的油气资源和潜力,盐构造控制着油气成藏和分布。其盐岩流动的不规律性,增加了盐构造的形成演化和演化期次分析的难度,前人主要通过平衡剖面恢复的方法对断裂等构造形态进行定量恢复,但对盐构造形成演化过程的认识及变形期次刻画的准确性明显不足。本文基于数值模拟手段,通过沉积地层的分时期加载方法,正演了下刚果盆地的构造演化过程,探讨并明确了盐构造的演化阶段。数值模拟结果表明,下刚果盆地盐构造的形成主要分为3个阶段:盐岩初始流动阶段、盐构造形成阶段和构造稳定阶段。形成底辟构造的主要时期是古新世-中新世。其中,古新世-渐新世开始形成底辟构造,中新世多个大规模底辟构造形成,且该时期是盐构造活动最强烈时期。在此基础上进一步完成了下刚果盆地盐构造活动变形与重力作用流动、上覆沉积地层厚度不均一以及沉积扇体的进积作用关系分析。
中图分类号:
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