Chemical equilibrium between ferropericlase and molten iron to 134 GPa and implications for iron content at the bottom of the mantle
(134GPaでのフェロペリクレースと溶融鉄の化学平衡およびマントル底における鉄含有量への影響)
NIMS author(s)
Fulltext and dataset(s) on Materials Data Repository (MDR)
Created at: 2016-05-24 15:27:32 +0900 Updated at: 2026-11-09 08:11:23 +0900