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机译:深层底层海外壳中富含型富相D和富含Al富含al的含水相的稳定性
Chinese Acad Sci Guangzhou Inst Geochem State Key Lab Isotope Geochem Guangzhou 510640 Guangdong Peoples R China;
Tokyo Inst Technol Dept Earth &
Planetary Sci Magma Factory Meguro Ku 2-12-1 Ookayama Tokyo 1528551 Japan;
Ehime Univ Geodynam Res Ctr 2-5 Bunkyo Cho Matsuyama Ehime 7908577 Japan;
Tokyo Inst Technol Dept Earth &
Planetary Sci Magma Factory Meguro Ku 2-12-1 Ookayama Tokyo 1528551 Japan;
Chinese Acad Sci Guangzhou Inst Geochem State Key Lab Isotope Geochem Guangzhou 510640 Guangdong Peoples R China;
Water; mantle transition zone; lower mantle; cold subduction; hydrous phases; basaltic crust;
机译:深层底层海外壳中富含型富相D和富含Al富含al的含水相的稳定性
机译:Ti-Al二元体系富Al部分中基于L1_0的有序相的相稳定性和互扩散性
机译:富铝γ-TiAl金属间化合物中Al 5 sub> Ti 3 sub>相中反相边界和反相畴的生长的蒙特卡罗模拟
机译:MCrAlY涂层与镍基基底相互扩散导致富铝储层形成的证据
机译:利用热力学相平衡建模约束底层海底外壳的构造热量演化
机译:含水海洋壳在低剪切应力下具有巨大的推力蠕变
机译:含有多个含水阶段的10至20 kbar的蒸汽不含熔化,可使多个含水阶段:对深层大陆地壳和活跃的大陆边缘的深度影响,对anatexis的影响