Volume 44 Issue 4
Apr.  2019
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Xie Qifeng, Cai Yuanfeng, Dong Yunpeng, Li Dunpeng, 2019. Zircon Geochronology and Hf Isotope Compositions of Biotite Granite in Southeast Ore Section of Zijinshan Ore Field, Fujian Province. Earth Science, 44(4): 1311-1326. doi: 10.3799/dqkx.2018.256
Citation: Xie Qifeng, Cai Yuanfeng, Dong Yunpeng, Li Dunpeng, 2019. Zircon Geochronology and Hf Isotope Compositions of Biotite Granite in Southeast Ore Section of Zijinshan Ore Field, Fujian Province. Earth Science, 44(4): 1311-1326. doi: 10.3799/dqkx.2018.256
shu

Zircon Geochronology and Hf Isotope Compositions of Biotite Granite in Southeast Ore Section of Zijinshan Ore Field, Fujian Province

doi: 10.3799/dqkx.2018.256
  • 1.

    College of Zijin Mining, Fuzhou University, Fuzhou 350108, China

  • 2.

    State Key Laboratory for Mineral Deposits Research, Nanjing University, Nanjing 210046, China

  • 3.

    State Key Laboratory of Continental Dynamics, Northwest University, Xi'an 710069, China

  • Received Date: 2018-08-21
  • Publish Date: 2019-04-15
    Abstract
  • Zijinshan ore field is located in the eastern part of South China fold system, belonging to the Southwest Fujian depression, where develops many large and super-large epithermal Au-Cu-Ag deposits which are closely related with magmatic activities. The study in this paper is based on a detailed research of the fine-grained biotite granite in the southeastern ore section including field geological survey and petrography, zircon rare earth elements, in-situ zircon U-Pb chronology and Hf isotope et al.. The LA-ICP-MS zircon U-Pb dating shows that the 206Pb/238U-207Pb/235U correlated age of the biotite granite is 109.5±1.9 Ma (MSWD=0.74, N=16), and 206Pb/238U weighed age is 107.44±0.94 Ma(MSWD=1.06, N=16), and the two ages are within the error range. According to zircon REE and magmatic oscillatory zoning characteristics and the Th/U ratios, the age can represent the rock crystallization age, which suggests fine-grained biotite granite emplaced in the Early Cretaceous of the Yanshanian epoch. The Hf isotope initial ratio εHf(t) values are negative, ranging from -4.99 to -1.06 (mean value is -2.99). Two stage Hf model ages (tDM2) range from 1 233.7 Ma to 1 485.4 Ma (mean value is 1 362.4 Ma). The εHf(t) and Hf values show small variations in distribution, which implies that magmatic rocks having a more uniform zircon Hf isotope composition. The in-situ zircon U-Pb chronology and Hf isotope show time and source characteristics of Early Cretaceous magmatic activity in south-western part of Fujian Province, which results from the evolution of the extension and thinning, and crust-derived magma substance involved from lithosphere are closely related. In this paper, it provides new evidence on the mineralization and tectonic evolution of the Zijinshan ore field.

     

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