在多晶钻石中记录的岩石层中的重新动员
1Institut fur Geologische Wissenschaften, Universitat Greifswald, F. -L. Jahnstrasse 17a, D-17487 Greifswald, Germany. DeBeers Geoscience Center, Post Office Box 82232, Southdale 2135, South Africa. Department of Geology, Royal Holloway Universi.
概括
来自南非的多晶钻石显示,在喷发前不久,旧的碳和酸盐材料被重新调动的证据. 这表明最近的钻石形成来自于克拉石层中的古老成分.
科学领域:
- 地质化学 地质化学
- 矿物学是一门学科.
- 石化学 石化学是一门学科.
背景情况:
- 金伯利特是火山岩,可以容纳钻石.
- 钻石的起源和形成过程是复杂的和有争议的.
- 了解钻石的形成,可以了解地球的深层过程.
研究的目的:
- 为了调查来自威尼斯金石的多晶钻石 (框架石) 的起源.
- 确定框架形成所涉及的时间和过程.
- 了解这些钻石中碳和酸盐成分的来源.
主要方法:
- 在框架内分析酸盐矿物质的同位素和微量元素特性.
- 石榴石中的化学变异与钻石中的碳同位素的相关性.
- 模拟生态石和碳酸盐化物之间的相互作用.
主要成果:
- 酸盐矿物质数据表明,旧的碳和酸盐成分的重新调动.
- 石榴石中的化学变异与钻石的碳同位素相关,这表明同时形成.
- 同位素和微量元素的变化与生态石碳酸盐融相互作用一致.
结论:
- 框架地形成于金伯利特喷发前不久,是由于石质层物质的重新动员而形成的.
- 钻石的形成涉及生态石和碳酸盐融之间的相互作用.
- 钻石是最近从古老的物质中形成的,这些物质储存在克拉顿石层中.
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