PAN Hui-bin, KANG Zhi-qiang, FU Wen-chun. 2014: SHRIMP zircon U-Pb ages of Xuwu subdacitic porphyry in the Dabaoshan ore district of northern Guangdong Province and its geological implications. Geological Bulletin of China, 33(6): 894-899.
    Citation: PAN Hui-bin, KANG Zhi-qiang, FU Wen-chun. 2014: SHRIMP zircon U-Pb ages of Xuwu subdacitic porphyry in the Dabaoshan ore district of northern Guangdong Province and its geological implications. Geological Bulletin of China, 33(6): 894-899.

    SHRIMP zircon U-Pb ages of Xuwu subdacitic porphyry in the Dabaoshan ore district of northern Guangdong Province and its geological implications

    • The Xuwu subdacitic porphyry is located in the south of the Dabaoshan ore district. This paper reports for the first time the SHRIMP zircon U-Pb age of Xuwu dacitic porphyry (441.2±4.2Ma), suggesting Caledonian. Combined with the previous dating results, the authors conclude that there are two rock-forming stages (Caledonian and Yanshanian) and one ore-forming stage (Yanshanian) in the Dabaoshan ore district, with the mineralization mainly related to the Yanshanian intrusions.
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