机译:自旋交叉和富含铁的硅酸盐在地球深部的地幔中融化
Department of Earth and Planetary Sciences, Tokyo Institute of Technology, Meguro, Tokyo 152-8551,Japan,Department of Earth and Planetary Sciences, University of Tokyo, Bunkyo, Tokyo 113-0033,Japan;
Department of Earth and Planetary Sciences, Tokyo Institute of Technology, Meguro, Tokyo 152-8551,Japan,Institute for Research on Earth Evolution, Japan Agency for Marine-Earth Scienceand Technology,Yokosuka.Kanagawa 237-0061,Japan;
Department of Earth and Planetary Sciences, Tokyo Institute of Technology, Meguro, Tokyo 152-8551,Japan;
Department of Earth and Planetary Sciences, Tokyo Institute of Technology, Meguro, Tokyo 152-8551,Japan,Institute for Research on Earth Evolution, Japan Agency for Marine-Earth Scienceand Technology,Yokosuka.Kanagawa 237-0061,Japan;
Department of Earth and Planetary Science, University of California, Berkeley, California 94720, USA;
Department of Materials, Physics and Energy Engineering, Nagoya University, Chikusa, Nagoya 464-8603, Japan;
National Synchrotron Radiation Research Center, Hsinchu 30076, Taiwan;
National Synchrotron Radiation Research Center, Hsinchu 30076, Taiwan;
机译:富含含水Fe的硅酸盐融化在地球的深层地幔中
机译:在地球深部上地幔的压力条件下,硅酸盐熔体的状态方程具有中等密度范围的中间范围
机译:在地球深部上地幔的压力条件下,硅酸盐熔体的状态方程具有中等密度范围的中间范围
机译:地幔源岩浆的隐晶中混溶的硫化物熔体的包裹体:对硅酸盐分馏过程中硫化物液体的演化的影响
机译:通过高压下降球粘度释放铁富含铁硅酸盐的粘度:对岩石粉质熔化的流动性的影响
机译:含碳硅酸盐在深地幔条件下熔融
机译:在地幔压力下硅酸盐在硅酸盐中润湿行为,具有对地球的深度碳循环的影响