水与地幔熔融(英文) | |
巫翔 | |
2015 | |
关键词 | mantle classic reservoirs magnesium geochemical geophysical oceanic implication dense subduction mantle classic reservoirs magnesium geochemical geophysical oceanic implication dense subduction |
英文摘要 | Water is one key factor to affect the chemical and physical properties of mantle materials,significant implication for geochemical,geophysical and geodynamical processes in the Earth’s mantle.Deeply subducted slabs of the oceanic lithosphere are proposed to transport amounts of water into the deep Earth,where dense hydrous magnesium silicates(DHMSs)are candidates of water reservoirs.Phase D,as a classic DHMS,is; Water is one key factor to affect the chemical and physical properties of mantle materials,significant implication for geochemical,geophysical and geodynamical processes in the Earth’s mantle.Deeply subducted slabs of the oceanic lithosphere are proposed to transport amounts of water into the deep Earth,where dense hydrous magnesium silicates(DHMSs)are candidates of water reservoirs.Phase D,as a classic DHMS,is; 中国地球物理学会、全国岩石学与地球动力学研讨会组委会、中国地质学会构造地质学与地球动力学专业委员会、中国地质学会区域地质与成矿专业委员会; 1 |
语种 | 英语 |
出处 | 2015中国地球科学联合学术年会 |
内容类型 | 其他 |
源URL | [http://ir.pku.edu.cn/handle/20.500.11897/489855] ![]() |
专题 | 地球与空间科学学院 |
推荐引用方式 GB/T 7714 | 巫翔. 水与地幔熔融(英文). 2015-01-01. |
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