跨晶体融化迁移和地球地幔的迁移
Pierre Schiano1, Ariel Provost, Roberto Clocchiatti
1Laboratoire Magmas et Volcans, Observatoire de Physique du Globe, Université Blaise Pascal et CNRS, 5 rue Kessler, 63038 Clermont-Ferrand Cedex, France. schiano@opgc.univ-bpclermont.fr
概括
岩内含物在热梯度下通过橄晶体迁移,由晶体融化相互作用驱动. 这解释了融分离,并质疑地球地幔中深层流体相.
科学领域:
- 地质化学 地质化学
- 地质物理学 地质物理学
- 矿物物理 矿物物理
背景情况:
- 板块构造学和火山活动是由岩和气体动力学驱动的.
- 了解地幔内的融化和气体行为对于火山运动和构造学至关重要.
研究的目的:
- 在热梯度下,研究结晶体内的融含的迁移机制.
- 了解融化迁移过程中溶解的气泡的行为.
- 将实验发现应用于大规模的地质过程,并重新评估深层流体阶段的存在.
主要方法:
- 实验室实验模拟了橄晶体内的融含物上的热梯度.
- 观察融化和气泡运动和相互作用.
- 结晶融化界面机制的动态分析.
- 将实验结果调整为地球地幔条件.
主要成果:
- 融化含有物通过橄晶体迁移,由晶体-融化界面动力学控制.
- 溶解后的气泡变得不动,并与迁移的融物分开.
- 实验结果解释了地幔中原始化的粒度分离.
- 含有富含二氧化碳的液体被重新解释为从融化中逃出的气体.
结论:
- 这项研究提供了一个在地幔内的粒度尺度上进行融分离的机制.
- 这些发现挑战了无处不在,深度透的自由流体相的概念.
- 融化迁移实验为在地质相关条件下的晶体生长动力学提供了见解.
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