H2 富含氧的鲁作为现代风格冷降温的指标
Mona Lueder1, Renée Tamblyn1, Daniela Rubatto1,2
1Institute of Geological Sciences, University of Bern, Baltzerstrasse 1+3, 3012 Bern, Switzerland.
概括
路提尔是一种类型的路提尔.
科学领域:
- 地质化学 地质化学
- 矿物学是什么?矿物学是什么?
- 石化学 石化学是一门学科.
背景情况:
- 路地质化学对于理解变态条件,年龄和石质学至关重要.
- 细性鲁分析有助于追踪过去的板块构造机制.
- 识别鲁中的压力依赖性微量元素是其作为地质计的应用的关键.
研究的目的:
- 研究鲁中的压力依赖性.
- 确定鲁中的H2O含量作为可行的压力指标.
- 开发方法来追踪rutile中的冷降温特征.
主要方法:
- 极化现场里叶变换红外光谱 (FTIR) 测量H2O含量.
- 对微量元素 (Nb,W,Sn,Zr,Fe) 和它们的比率 (H2O/Zr,Fe/Zr) 的分析.
- 使用区分图来进行岩石学识别.
主要成果:
- 鲁中的H2O含量与峰值变态压力相关,作为压力指标.
- 在低温生态石面中观察到的最高H2O度是来自寒冷俯冲区的鲁.
- 用FTIR绘图显示的低于600-700°C的保持率.
- H2O/Zr和Fe/Zr的比率可以指示热梯度,并识别特定的鲁类型.
- Nb,W和Sn的含量区分了宿主/来源石质.
结论:
- 鲁中的H2O是一种可靠的转化压力指标.
- 结合地质化学代理 (H2O/Zr,微量元素) 可以识别鲁中的冷降温特征.
- 这些发现使得能够追踪古老的冷降温事件在破碎物记录中.
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