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《Geotectonica Et Metallogenia》 2012-02
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LA-ICP-MS Zircon U-Pb Dating of the Dacite Porphyry from Zijinshan Cu-Au Deposit and its Metallogenetic Implications

HU Chunjie1,2, HUANG Wenting1,2, BAO Zhiwei1, LIANG Huaying1 and WANG Chunlong1,2 (1.CAS Key Laboratory for Mineralogy and Metallogeney, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, Guangdong, China; 2.Graduate University of Chinese Academy of Sciences, Beijing 100049, China)  
The dacite porphyry occurs in the volcanic caldera of Zijinshan ore field and closely associates with the Cu-Au mineralization. The LA-ICP-MS zircon U-Pb dating of two dacite porphyry samples yields weighted mean ages of (105.0±0.7)Ma and (105.0±2.2)Ma, respectively. These results suggest that the dacite porphyry was formed proximately contemporarily with the other two Mo and Cu mineralized granite porphyries, i.e., the Sifang and Luoboling granite porphyries. The dacite and granite intrusives are characterized by high Ce4+/Ce3+ ratios, which indicates that the magmatic system was of oxidative and therefore consistent with the huge Cu-Mo-Au ore-forming potential of the dacite and granite porphyries. Moreover, the similarities of age, geochemical characteristics and mineralization demonstrate that the Cu-Mo-Au mineralization in the Zijinshan ore field is most likely a unified porphyry ore-forming system.
【Fund】: 国土资源部深部矿产资源立体探测技术及实验研究(SinoProbe-03-01);; 中国科学院重大项目(KZCX1-YW-15-3);; 国家自然科学基金项目(41172080 41121002)资助
【CateGory Index】: P612
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