High-P/T experimental studies and water in the silicate mant

发布时间：2020-12-16 05:08

　　Water（or H） in the silicate mantle is a key element in influencing Earth’s climate, habitability, geochemical evolution, geophysical properties and geodynamical processes, and has received increasing attention in the past decades. Experimental work under simulated high-pressure and high-temperature conditions is a powerful tool in characterizing the species, distribution, storage capacity and various physicochemical impacts of water in the mantle. In recent years, significant approaches have bee... 

【文章来源】：Science China(Earth Sciences). 2016年04期

【文章页数】：13 页

【文章目录】：
1. Introduction
2. High-pressure and temperature experiments
3. Water in the silicate mantle
    3.1 Origin of water in the mantle
    3.2 Water in the mantle
    3.3 Mantle storage capacity of water
4. Effects of water on mantle properties
    4.1 D/H ratios between the mantle and oceans
    4.2 Water and partial melting in the mantle
    4.3 Water and electrical conductivity of the mantle
    4.4 Water and rheology of the mantle
5. Conclusions


【参考文献】：
期刊论文
[1]浅谈高温高压实验地球科学:方法和应用[J]. 杨晓志.  矿物岩石地球化学通报. 2015(03)



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