机译:花岗岩系统在800-900℃和100-200 MPa下的扩散控制熔融:花岗岩熔体中最小扩散率的温度和压力依赖性
Department of Earth and Environmental Sciences, School of Science, Graduate School of Science and Technology, Kumamoto University, 2-39-1, Kurokami, Kumamoto 860-8555, Japan Mizunami Underground Research Laboratory, Geological Isolation Research and Development Directorate, Japan Atomic Energy Agency,1-64, Yamanouchi, Akeyo, Mizunami, Gifu 509-6132, Japan;
Department of Earth and Environmental Sciences, School of Science, Graduate School of Science and Technology, Kumamoto University, 2-39-1, Kurokami, Kumamoto 860-8555, Japan;
Department of Earth and Environmental Sciences, School of Science, Graduate School of Science and Technology, Kumamoto University, 2-39-1, Kurokami, Kumamoto 860-8555, Japan;
Department of Earth and Environmental Sciences, School of Science, Graduate School of Science and Technology, Kumamoto University, 2-39-1, Kurokami, Kumamoto 860-8555, Japan;
Department of Earth and Environmental Sciences, School of Science, Graduate School of Science and Technology, Kumamoto University, 2-39-1, Kurokami, Kumamoto 860-8555, Japan;
Department of Earth and Environmental Sciences, School of Science, Graduate School of Science and Technology, Kumamoto University, 2-39-1, Kurokami, Kumamoto 860-8555, Japan;
diffusion-controlled melting; minimum diffusivity in the melt; granitic system; parabolic growth rate law; melting experiments;
机译:花岗岩系统中800-900°C和100-200 MPa时扩散控制的熔化:花岗岩熔体中最小扩散率的温度和压力依赖性
机译:辉钼矿在800℃,100-200 MPa含水花岗岩熔体中的溶解度
机译:在800°C和200 MPa的H 2 sub> O饱和单斜晶质熔体中石英,阿尔比特和正长石的溶解:地壳南极条件下花岗质熔体的扩散运移特性
机译:钨和锡轴承花岗岩熔体在850℃和150MPa下饱和水的液体
机译:高温高压下长石与水的体系中熔融和矿物溶解度的实验研究,特别是花岗岩的来源
机译:{x1 C4mim MeSO4 +(1−x1)MeOH}系统在(283.15至333.15)K温度和(0.1至35)MPa压力下的体积性质
机译:在800-900°C和100-200MPa的花岗岩系统中扩散控制熔化:花岗岩熔体中最小扩散率的温度和压力依赖性