ZHANG Yue, LI Xiangmin, PAN Feng, SONG Zhongbao. 2018: LA-ICP-MS zircon U-Pb dating of the porphyaceous syenogranite in Niuxinshan along the central segment of North Qilian orogenic belt and its geological significance. Geological Bulletin of China, 37(4): 724-733.
    Citation: ZHANG Yue, LI Xiangmin, PAN Feng, SONG Zhongbao. 2018: LA-ICP-MS zircon U-Pb dating of the porphyaceous syenogranite in Niuxinshan along the central segment of North Qilian orogenic belt and its geological significance. Geological Bulletin of China, 37(4): 724-733.

    LA-ICP-MS zircon U-Pb dating of the porphyaceous syenogranite in Niuxinshan along the central segment of North Qilian orogenic belt and its geological significance

    • The porphyaceous syenogranite pluton is exposed in the west of Qilian Country, Qinghai Province. The authors conduct-ed LA-ICP-MS zircon U-Pb dating of the porphyaceous syenogranite and the result shows that the age is 166.6±2.4Ma, suggesting the Middle Jurassic of Yanshanian period. Several inheritable magmatic zircons yielded the age information of the Precambrian peri-od. Geochemical data show that the porphyaceous syenogranite is silica-enriched in composition with high content of alkali, and hence it is a peraluminous granite and belongs to the high-K calc-alkaline series. It is characterized by enrichment of Rb, Th, K, de-pletion of Ba, Nb, P, Ti, and weak negative anomaly of Eu, with the average Rb/Sr ratio being 1.86, which reflects the characteris-tics of the crust source and indicates S type granite.
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