在橄和染色体中因元素扩散而产生的异常融含体的生存时间
C Spandler1, H St C O'Neill, V S Kamenetsky
1Research School of Earth Sciences, Australian National University, Canberra 0200, Australia. spandler@geo.unibe.ch
Nature
|May 18, 2007
概括
奥利文和克罗米特中的融化含量不会保存早期地幔融化成分. 稀土元素在岩温度下的快速扩散,使喷发前的含有物重新平衡.
科学领域:
- 地质化学 地质化学
- 石化学 石化学是一门学科.
- 地球科学 地球科学 地球科学
背景情况:
- 岩岩的组成是由复杂的地幔和地过程造成的.
- 在晶体 (奥利文,克罗米特) 中的融化含有物被研究以了解早期地幔融化的起源.
- 异常的融化纳入组合通常被解释为未经修改的地幔融化.
研究的目的:
- 为了测试融化纳入保护早期地幔融化成分的假设.
- 为了研究岩上升和演化过程中融化的化学隔离.
- 重新评估融内含物中异常微量元素特征的解释.
主要方法:
- 在岩温度下研究了稀土元素 (REE) 在奥利文和克罗米特中的扩散.
- 将扩散时间尺度与岩产量和上升时间尺度进行比较.
- 在phenocryst托管的融含物中分析了微量元素模式.
主要成果:
- 在岩温度下,Olivine和Chromite中的REE的晶格扩散是快速的.
- 融化中的REE模式迅速重新平衡,在比岩上升更短的时间尺度内.
- 异常的微量元素标志在喷发接近时形成,不反映早期地幔过程.
结论:
- 对于融物中不兼容元素的化学隔离假设是无效的.
- 晶托管的融化含有物不会保存原始的地幔融化成分.
- 需要重新评估关于地幔异质性的融化纳入解释.
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