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《Geology in China》 2015-02
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LA-ICP-MS zircon U-Pb dating and geological features of Changxing intrusion in the Hebaoshan gold deposit, Taining County, Fujian Province

CHEN Guo-jian;ZHANG Wei-bo;LIU Jiang-Tao;North Fujian Geological Party;Development and Research Center,China Geological Survey;  
The Changxing potash feldspar migmatitic granite is related to the mineralization in the Hebaoshan gold deposit. The mineralization in the Hebaoshan gold deposit shows multi- period and multi- stage characteristics, and the intrusion activities of Changxing potash feldspar migmatitic granite in the late Caledonian promoted the early period migration and enrichment of the oreforming elements in the gold deposit and the tectonic- magmatic activity of the late Indosinian to early Yanshanian superimposed mineralization. The authors made a detailed chronological study of the main intrusive rocks formed in the Caledonian period. Insitu zircon U- Pb dating was performed with LA-ICP-MS, and reliable n(206Pb)/n(238U) age data of zircons were obtained. The results yielded concordant age of(437.1 ± 1.3) Ma for potash feldspar migmatitic granite,(436.6 ± 1.1) Ma for biotite quartz diorite and(427.1 ± 1.4) Ma for biotite granite diorite vein. The age data constrain the upper limitation of the metallogenic period, thus having great geological implications for further mineralization research.
【Fund】: 中国地质调查局项目(1212011085534)资助
【CateGory Index】: P597.3;P618.51
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