概括
庞盖亚和大西洋形成的分裂涉及地幔动力学和大陆地在1亿年内蔓延. 摩洛哥 摩洛哥 摩洛哥 摩洛哥 摩洛哥 摩洛哥
科学领域:
- 地质地质地质地质地质地
- 构造学 构造学 构造学 构造学
- 地力学是什么?地力学是什么?
背景情况:
- 庞盖亚超大陆的分裂和大西洋的形成是由地幔动力学和地的扩散驱动的.
- 摩洛哥大陆地保留了这些构造事件的详细记录.
研究的目的:
- 为了分析地在庞盖亚分裂期间对地幔动态的地反应.
- 了解大西洋形成的时间和机制.
- 为了研究晚期古老生态或生成在启动中生态裂变中的作用.
主要方法:
- 分析摩洛哥地的结构和沉积模式.
- 解释地质数据以重建过去的构造压力和环境.
主要成果:
- 非洲边缘在罗纪中期稳定成为海洋碳酸盐环境.
- 早期中生代的拉力应力创造了两个断层系统和一个盆地和范围的结构风格.
- 晚期古老时代的变形和入侵先于中世时代的扩散事件.
结论:
- 地幔动力学需要超过1亿年的时间来促进潘盖亚的分裂和大西洋的形成.
- 晚期古老时代的热态发育可能已经启动了传播中心发展的早期阶段.
- 摩洛哥地提供了大陆对地幔驱动裂的反应的全面记录.
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