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北祁连的形成与演化历史:来自河流沉积物地球学及其碎屑锆石U-Pb年龄、Hf同位素组成的证据
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摘要
<正>河流沉积物中碎屑锆石U-Pb定年与Hf同位素分析相结合可获得所研究区域地壳的形成、演化的丰富信息,细粒沉积物是对流经源区的地壳进行均匀采样的理想工具(Taylor et al.,1985、1995;Mc Lennan.,2001;Rudnick et al.,2004;Bodet et al.,2000;Luo et al.,2008;陈岳龙等,2014)。在北祁连造山带中,发源于西北端的北大河,中部的梨园河、黑河,东南部的西大河、东大河、
引文
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