在前坎布里亚板块构造过程中构建克拉顿基尔
A L Perchuk1,2, T V Gerya3, V S Zakharov4
1Geological Faculty, Lomonosov Moscow State University, Moscow, Russia. alp@geol.msu.ru.
Nature
|October 15, 2020
概括
古老的大陆核心 (巨) 具有由前坎布里亚时代的沉降形成的深层地幔. 这一过程创造了厚厚的石化层,对于岩的生存和钻石的形成至关重要.
科学领域:
- 地质学
- 地质学
- 构造学
背景情况:
- 克拉顿是古老的大陆核心,
- 地幔基尔是隔离的,耗尽的,浮动的,含有钻石的地幔体积.
- 基尔形成仅发生在早期地球 (1.5-3.5亿年前) 并且缺乏现代类型.
研究的目的:
- 调查层层地带基尔的起源.
- 探索早期地球构造学在基尔形成中的作用.
- 了解克拉顿长寿的条件.
主要方法:
- 模拟了海洋沉积和弧形大陆碰撞.
- 模拟了地球地幔早期温度的升高 (150-250°C以上).
- 分析了原始的位置和冷却动态.
主要成果:
- 热,浮动的地下层地幔在引板下没有引.
- 石板留下了克拉尺度的原始岩石.
- 原岩层的厚度与岩层的最大年龄相关.
结论:
- 在甲纪前,海洋板块的沉积形成了层层的地幔.
- 这种机制解释了基尔层和克拉顿的生存.
- 随后的冷却使得钻石形成.
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