潮湿的岩固体和海洋地幔潜在温度的实验约束
Emily Sarafian1,2, Glenn A Gaetani2, Erik H Hauri3
1Massachusetts Institute of Technology-Woods Hole Oceanographic Institution Joint Program in Oceanography/Applied Ocean Science and Engineering, Cambridge, MA 02139, USA. etursack@whoi.edu.
概括
在海洋上层地幔中溶解的水 (H2O) 显著提高了矿固体的温度. 这一发现需要对海洋扩散中心下地幔上升的潜在温度估计进行上调.
科学领域:
- 地质化学
- 地质学
- 矿物物理
背景情况:
- 海洋地是由扩散中心下方的上升地的解压融化产生的.
- 在名义上无水地幔矿物中溶解的水 (H2O) 对点 (固体) 有着显著的,但未经实验量化的影响.
研究的目的:
- 通过实验确定溶解对矿固体的影响.
- 量化H2O对地幔化的影响.
主要方法:
- 在受控的H2O度下实验测定矿.
- 在地幔中进行高温和高压实验.
主要成果:
- 经过实验证明,H2O不和的矿比之前估计的要高.
- 溶解的H2O的存在显著地提高了矿融化的温度.
结论:
- 海洋地幔融化的现有模型可能低估了所需的潜在温度.
- 东太平洋上升下的地质观测表明,海洋上层地幔的潜在温度估计上升了60°C.
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