论文信息 - Trace element partitioning between majoritic garnet and silicate melt at 10-17 GPa: Implications for deep mantle processes - 字舞流文

Trace element partitioning between majoritic garnet and silicate melt at 10-17 GPa: Implications for deep mantle processes

W. McDonough | Y. Fei | W. Minarik | Karen Moreno | A. Corgne | S. Keshav | L. Armstrong | Alexandre Corgne