概括
南非的Kaapvaal石坑有一个深层地幔根的枯竭的石,形成超过30亿年前. 这种古老的形根很可能是阿克海时期钻石形成的宿主.
科学领域:
- 地质物理学 地质物理学
- 地质化学 地质化学
- 矿物学是什么?矿物学是什么?
背景情况:
- 位于非洲南部的卡普瓦尔 (Kaapvaal) Kraton 保持着一个深层岩层根.
- 了解克拉顿根提供了对地球早期地质过程的见解.
研究的目的:
- 为了描述卡普瓦尔石坑的地幔结构.根.
- 确定克拉顿根的热和组成演变.
主要方法:
- 从金贝莱石中分析钻石内含物,晶和石.
- 地质和地化学数据的解释.
主要成果:
- 卡普瓦尔石坑的地幔根主要由岩贫的岩石组成.
- 天气层边界在克拉顿和周围的移动带下面的深度有所不同.
- 根的形成早于30亿年前,温度为900~1200°C.
结论:
- 卡普瓦尔石坑的根是一个古老的,热稳定的岩层结构.
- 在非洲南部发现的钻石很可能在这个古老的岩根中结晶.
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