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Geochronology and Geochemistry of Zengga Mesozoic Grantoids from East Gangdese Batholith, Implications for the Remelting Mechanism of Granite Formation 被引量:3

Geochronology and Geochemistry of Zengga Mesozoic Grantoids from East Gangdese Batholith, Implications for the Remelting Mechanism of Granite Formation
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摘要 This paper reports geochemistry (major and trace elements), zircon U-Pb and Lu-Hf isotope studies of leucogranite, granodiorite and clinopyroxene-bearing diorite from the Zengga intrusive body, eastern Gangdese batholith, Tibet. Massive granodiorite is mainly composed of fine- and medium-grained plagioclase (65 modal %), This paper reports geochemistry (major and trace elements), zircon U-Pb and Lu-Hf isotope studies of leucogranite, granodiorite and clinopyroxene-bearing diorite from the Zengga intrusive body, eastern Gangdese batholith, Tibet. Massive granodiorite is mainly composed of fine- and medium-grained plagioclase (65 modal %),
出处 《Acta Geologica Sinica(English Edition)》 SCIE CAS CSCD 2015年第A02期113-114,共2页 地质学报(英文版)
基金 funded by the Key project of national natural science funds (40930313) Chinese Geological Survey Project Funds (12120114061801, 12120114057701 and 12120114061501)
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