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- W2365807846 abstract "The Bashierxi pluton is located in the western segment of the eastern Kunlun,between Baiganhu fault and Aerjin fault,this pluton mainly consists of monzonitic granite and K-feldspar granite,and the monzonitic granite is closely related with the ore-forming process of the Baiganhu tungsten-tin deposit.The internal structures,cathodeluminescence(CL) images and Th/U ratios of the zircon grains from the monzonitic granite reveal that these zircon grains have typical characteristics of magmatic zircon.The LA-ICP-MS analyses show that the zircon grains from the monzonitic granite have concordant U-Pb ages of(458.0±9.0)Ma,on the other hand,the zircon grains from the K-feldspar granite have U-Pb ages of(432.3±0.8)Ma,these data indicated that the Bashierxi pluton is a intrusion formed from Late Ordovician to Early Silurian.Major and trace element data of the monzonitic granite show that Bashierxi granite is weakly metaluminous or peraluminous A-type granite.These rocks were considered as melts derived from crustal source during back-arc basin extension in eastern Kunlun,and the early Baiganhu tungsten-tin deposit era is represented by the ages of monzonitic granite." @default.
- W2365807846 created "2016-06-24" @default.
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- W2365807846 date "2010-01-01" @default.
- W2365807846 modified "2023-09-23" @default.
- W2365807846 title "Zircon LA-ICP-MS U-Pb dating and geological significance of Bashierxi granite in the eastern Kunlun area,China" @default.
- W2365807846 hasPublicationYear "2010" @default.
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