在石化层与石化层边界的水性融化的羽毛起源
Daniel Blatter1,2, Samer Naif3, Kerry Key4
1Lamont-Doherty Earth Observatory, Columbia University, Palisades, NY, USA. dblatter@ucsd.edu.
Nature
|April 21, 2022
概括
在构造板下面的柔性天气层的起源是有争议的. 我们的研究表明地幔羽毛替代了富含挥发性物质的融化物,
科学领域:
- 地质学
- 构造学
- 地幔动力学
背景情况:
- 板块构造学依赖于石化层-石化层边界 (LAB) 下的低粘度的石化层.
- 这种柔性层的起源是有争议的,其中包括温度,水合或部分化的原因.
- 之前的研究没有同时考虑融稳定性和电阻性不确定性.
研究的目的:
- 调查 LAB 的低粘度通道的来源.
- 在LAB通道内限制融分数和挥发性含量.
- 确定对地幔羽毛活动的影响.
主要方法:
- 结合实验约束的地幔化参数与挥发性存在.
- 应用贝叶斯电阻逆转到来自可可板的磁电流数据.
- 融化的综合热力学稳定性与电阻估计.
主要成果:
- 导电性LAB通道需要大量的化物或大量的挥发物.
- 大量的融化分量在机械上不稳定,与迁移模型相冲突.
- 这些发现表明地幔羽毛将富含挥发物质的融物置于LAB通道中.
结论:
- 道的特征指向一个地幔羽毛源.
- 这可能是来自加拉帕戈斯热点的前所未知的风云或影响.
- 水性融道可能是LAB异常的广泛来源.
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