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... 

【文章來源】：Science China(Earth Sciences). 2016年04期

【文章頁數(shù)】：13 頁

【文章目錄】：
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


【參考文獻(xiàn)】：
期刊論文
[1]淺談高溫高壓實(shí)驗(yàn)地球科學(xué):方法和應(yīng)用[J]. 楊曉志.  礦物巖石地球化學(xué)通報(bào). 2015(03)



本文編號(hào)：2919586