Reaction experiments between tonalitic melt and mantle olivine and their implications for genesis o

• 作 者: WANG MingLiang TANG HongFeng
• 机 构: Laboratory.forHighTemperature&,HighPressureStudyoftheEarth',sInterior,UniversityofChineseAcade
• 出 处: 中国科学：地球科学英文版
• 发表日期: 2013年11期
• 关键词: 高镁安山岩 地幔橄榄岩 实验模拟 克拉通 熔体 反应 成因意义 地球化学调查 tonalitic melt mantle olivine melt-mine
• 基金项目: supported by the Knowledge Innovation Program of the Chinese Academy of Sciences(Grant No.KZCX2-YW-Q08-3-4),the project from the State Key Laboratory for Mineral Deposits Research,Nanjing University(G

High-Mg(Mg#>45)andesites(HMA)within cratons attract great attention from geologists.Their origin remains strongly debated.In order to examine and provide direct evidence for previous assumptions about HMA’s genesis inferred from petrological and geoche