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Petrogenesis of the Late Triassic diorites in Hohxil, northern Tibet: Fractional crystallization of primitive andesitic magmas and insights into the origin of high-Mg# andesitic signature of the continental crust
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摘要
<正>An integrated study of petrology,whole-rock and Sr–Nd isotope compositions,combined with zircon U–Pb ages and Hf isotopes,for the Wudaoliang diorites from the Hohxil area,northern Tibet provides constraints on the genesis of intermediate magmas and insights into the origin of high-Mg# andesitic signature of the continental crust.LA-ICP-MS zircon U-Pb dating indicates that the Wudaoliang diorites were generated in
引文
Kelemen,P.B.Genesis of high Mg#andesites and the continental crust.Contributions to Mineralogy and Petrology,1995,120(1):1-19.
    Rudnick,R.L.,Gao,S.Composition of the continental crust.Treatise on Geochemistry,2003,3:1-64.
    Tatsumi,Y.High-Mg andesites in the Setouchi volcanic belt,southwestern Japan:analogy to Archean magmatism and continental crust formation?Annual Review of Earth and Planetary Sciences,2006,34:467-499.
    Wang,Q.,Li,Z.X.,Chung,S.L.,et al.Late Triassic high-Mg andesite/dacite suites from northern Hohxil,North Tibet:Geochronology,geochemical characteristics,petrogenetic processes and tectonic implications.Lithos,2011,126(1-2):54-67.

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