在地球的中年时代产生的静止
概括
地球山脉形成的历史显示,在古世和世时代,地的厚度最高. 由于超级大陆的存在,原生态时期的山脉活动有所减少,这可能阻碍了生命的进化.
科学领域:
- 地质学
- 地质化学
- 古生物学
背景情况:
- 山地带对于营养循环至关重要,影响排泄和水文.
- 了解长期的山脉形成过程是地球表面演变的关键.
研究的目的:
- 用地化学代理来重建山脉形成的历史.
- 研究大陆地的厚度与地质时间上的活动之间的关系.
主要方法:
- 作为追踪山脉形成的替代物,
- 分析了地质时代的活跃大陆地厚度的变化.
主要成果:
- 大陆地的厚度在阿纪和法内罗纪时期达到顶峰.
- 原生态时代表现出地厚度的持续下降,与最小的orogenesis.
- 长期的原生态静止与Nuna-Rodinia超大陆有关.
结论:
- 超大陆周期对地幔的热结构和岩层强度产生重大影响,影响了山脉的形成.
- 在前世时期缺乏重要的山脉形成可能导致海洋营养物质的限制和进化进程的停滞.
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