典型文献
Dense hydrous silica carrying water to the deep Earth and promotion of oxygen fugacity heterogeneity
文献摘要:
Water has remarkable effects on the properties of mantle rocks,but,owing to the high temperatures in the mantle,uncertainties remain about how and how much water is transported into the deep Earth.Recent studies have shown that stishovite and post-stishovites as high-pressure phases of SiO2 have the potential to carry weight percent levels of water into the Earth's interior along the geotherm of the subducting oceanic crust.As slabs are subducted to the deepest mantle,dehydration of these dense hydrous silica phases has the potential to change the physicochemical properties of the mantle by reducing melting points,forming new high-pressure phases,and enhancing the oxygen fugacity heterogeneity of the lower mantle.
文献关键词:
中图分类号:
作者姓名:
Yanhao Lin;Ho-Kwang Mao
作者机构:
Center for High Pressure Science and Technology Advanced Research,Beijing 100193,People's Republic of China
文献出处:
引用格式:
[1]Yanhao Lin;Ho-Kwang Mao-.Dense hydrous silica carrying water to the deep Earth and promotion of oxygen fugacity heterogeneity)[J].极端条件下的物质与辐射(英文),2022(06):76-78
A类:
stishovite,stishovites
B类:
Dense,hydrous,silica,carrying,water,Earth,promotion,oxygen,fugacity,heterogeneity,Water,remarkable,effects,properties,mantle,rocks,but,owing,high,temperatures,uncertainties,remain,about,much,transported,into,Recent,studies,have,shown,that,post,pressure,phases,SiO2,potential,weight,percent,levels,interior,along,geotherm,subducting,oceanic,crust,slabs,are,subducted,deepest,dehydration,these,dense,change,physicochemical,by,reducing,melting,points,forming,new,enhancing,lower
AB值:
0.568172
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