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富氟花岗质熔体形成和演化的实验研究
引用本文:李福春,朱金初,等.富氟花岗质熔体形成和演化的实验研究[J].岩石学报,2003,19(1):125-130.
作者姓名:李福春  朱金初
作者单位:1. 南京农业大学资源与环境科学学院,南京,210095;南京大学地球科学系,成矿作用国家重点实验室,南京,210093
2. 南京大学地球科学系,成矿作用国家重点实验室,南京,210093
基金项目:国家自然科学基金(49873017),高校博士点基金(199902842)
摘    要:通过高温高压实验,模拟了富氟花岗质熔体形成和演化的过程,结果表明,随着结晶分异作用的进行,熔体中SiO2含量降低而Al2O3和F含量升高,相应地,A/NKC和NKA/Si比值逐渐升高,并最终形成了贫硅过铝富氟的熔体。

关 键 词:花岗质熔体  形成  溶化  高温高压实验    结晶分异作用
文章编号:1000-0569/2003/019(01)-0125-30
修稿时间:2002年2月25日

Experimental study on formation and evolution of F-rich granitic melt.
LI FuChun,ZHU JinChu,ZHANG LinSong,RAO Bing and ZHANG PeiHua . College of Resources and Environmental Sciences,Nanjing Agricultural University,Nanjing,China.Experimental study on formation and evolution of F-rich granitic melt.[J].Acta Petrologica Sinica,2003,19(1):125-130.
Authors:LI FuChun  ZHU JinChu  ZHANG LinSong  RAO Bing and ZHANG PeiHua College of Resources and Environmental Sciences  Nanjing Agricultural University  Nanjing  China
Institution:LI FuChun,ZHU JinChu,ZHANG LinSong,RAO Bing and ZHANG PeiHua . College of Resources and Environmental Sciences,Nanjing Agricultural University,Nanjing,China. Department of Earth Sciences and State Key Laboratory for Mineral Deposits Research,Nanjing University,Nanjing f China
Abstract:Through high T-P experiments, the process of generation and evolution of F-rich granitic melt had been studied. The results demonstrate that along with crystallization of granitic magma, SiO2 in the residual melt decrease, while Al2O3 and F increase which results in both A/NKC and NKA/Si rations to be increased, and finally poor-Si peraluminous F-rich granite melt to be formed. This is in good agreement with vertical petrochemical zonation observed in natural Li-F-rich granites.
Keywords:Granitic melt  Formation  Evolution  High T-P  Experiment
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