Journal of Jilin University(Earth Science Edition) ›› 2020, Vol. 50 ›› Issue (5): 1462-1490.doi: 10.13278/j.cnki.jjuese.20190308

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Zircon U-Pb Age and Hf Isotope of Multiple-Stage Magmatism and Mineralization in Lianhuashan Region, Eastern Guangdong

Fan Feipeng1, Xiao Huiliang1, Chen Lezhu1, Li Haili1, Liu Jianxiong2, Deng Zhonglin2, Kang Congxuan1, Lin Gengwei3, Chen Kai4   

  1. 1. Nanjing Center, China Geological Survey, Nanjing 210016, China;
    2. Guangdong Foshan Geological Bureau, Foshan 528000, Guangdong, China;
    3. Guangdong Second Geological Brigade, Shantou 515000, Guangdong, China;
    4. College of Resources and Geosciences, China University of Mining and Technology, Xuzhou 221000, Jiangsu, China
  • Received:2019-07-20 Online:2020-09-26 Published:2020-09-29
  • Supported by:
    Supported by Project of China Geological Survey (12120114015701, DD20190153,DD20160037) and National Key R & D Program of China (2016YFC0600210)

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Abstract: Lianhuashan region is located in the continental volcanic area of the southeast coast of China, which is an important prospecting area for tungsten-gold mineralization. The authors studied the zircon U-Pb age, granite geochemistry, zircon trace elements, and Hf isotope of the newly found Mesozoic intrusive rocks in Lianhuashan region in the southeast coastal areas of China, and identified three stages magmatism: Middle Jurassic quartz diorite porphyries ((168.0±2.2) Ma), early stage of Early Cretaceous biotite monzonites( (137.5±1.9)Ma), and late stage of Early Cretaceous quartz porphyries ((102.0±1.5) Ma and (98.7±1.8) Ma). The intrusive rocks belong to calc-alkaline, aluminous, strong-peraluminous magmatic rocks. The quartz porphyry and rhyolite porphyry are closely related to the mineralization. The 176Lu/177Hf values of all magmatic zircons are less than 0.002, the 176Hf/177Hf values are mostly less than 0.282 7. The zircon Hf isotope values of εHf(t) are mostly between -2.57 and 1.00, fLu-Hf values are in the range of -0.99-0.95, and their corresponding crustal model ages (TDM2) are mainly 1.00-0.81 Ga, which indicates that the source of diagenetic materials were derived from the partial melting of metamorphic mudstones and metamorphic sands of Neoproterozoic in the lower crust, and mixed with small amount of mantle material. The crystallization temperatures of zircons are mostly in the range of 650-750 ℃, which shows the characteristics of I-type granite. In combination with all these data, the magmatism and mineralization of Lianhuashan region are closely related to the tectonic transformation event. Although there is no high-precision metallogenic age to limit the time of metallogeny, the tungsten-gold mineralization time should be slightly later than the formation time of the quartz porphyry (ca. 102.0-98.7) according to the geological facts and this study results.

Key words: granites, LA-ICP-MS zircon U-Pb dating, Lu-Hf isotope, mineralization, Lianhuashan tungsten-gold deposit, Lianhuashan region,eastern Guangdong

CLC Number: 

  • P588.12
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