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Cretaceous–Cenozoic tectonic history of the Jiaojia Fault and gold mineralization in the Jiaodong Peninsula, China: constraints from zircon U–Pb, illite K–Ar, and apatite fission track thermochronometry
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  • 作者:Jun Deng ; Changming Wang ; Leon Bagas ; Emmanuel John M. Carranza…
  • 关键词:Zircon U–Pb dating ; Apatite fission track ; Illite K–Ar age ; Tectonic implications ; Jiaojia Fault ; Tan ; Lu Fault ; Jiaodong Peninsula
  • 刊名:Mineralium Deposita
  • 出版年:2015
  • 出版时间:December 2015
  • 年:2015
  • 卷:50
  • 期:8
  • 页码:987-1006
  • 全文大小:18,794 KB
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  • 作者单位:Jun Deng (1)
    Changming Wang (1) (2)
    Leon Bagas (2)
    Emmanuel John M. Carranza (3)
    Yongjun Lu (2)

    1. State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, No. 29, Xueyuan Road, Haidian District, 100083, Beijing, China
    2. Centre for Exploration Targeting and Australian Research Council Centre of Excellence for Core to Crust Fluid Systems (CCFS), School of Earth and Environment, University of Western Australia, Perth, WA, 6009, Australia
    3. School of Earth and Environmental Sciences, James Cook University, Townsville, Queensland, Australia
  • 刊物类别:Earth and Environmental Science
  • 刊物主题:Earth sciences
    Geology
    Mineral Resources
    Mineralogy
  • 出版者:Springer Berlin / Heidelberg
  • ISSN:1432-1866
文摘
The Jiaojia Fault (JJF) in the Jiaodong area of eastern China is an important NNE-trending structure that is subsidiary to the regional Tancheng–Lujiang (Tan-Lu) Fault Zone, and hosts >1200 t of gold reserves contained in disseminated and stockwork ore, dominantly in the footwall of the fault. We present new zircon U–Pb, apatite fission track, and illite K–Ar data along the JJF and have delineated its tectonic history focusing on its formation and reactivation. Zircon U–Pb dating shows that the Shangzhuang granite is a composite body with ages between 132?±- and 127?±- Ma. Illite K–Ar ages for the fault’s gouge range from 83?±- to 68?±- Ma, and the measured apatite fission track ages for ores are between 55 and 21 Ma. Previous zircon U–Pb geochronology and structural studies suggest that the JJF was originally activated in the Jurassic during 160-50 Ma as a sinistral fault. The JJF was a normal fault in the Early Cretaceous due to NW–SE orientated tension and NE–SW compression, which lasted from 135 to 120 Ma. This was followed by sinistral strike–slip faulting due to NW–SE compression and NE–SW tension during 120-10 Ma, and it changed to normal displacement at ca. 110 Ma. Our apatite fission track data analysis and thermal modeling of representative samples suggest that there was a subsequent dextral reactivation of the fault at ca. 55 Ma. Previous age data of ca. 130-10 Ma for gold mineralization along the JJF coincides with the Early Cretaceous magmatism and is coeval with the transition from normal faulting to sinistral strike–slip faulting of the JJF in Early Cretaceous, which is interpreted to be due to changing direction of the subducting Pacific Plate. Keywords Zircon U–Pb dating Apatite fission track Illite K–Ar age Tectonic implications Jiaojia Fault Tan-Lu Fault Jiaodong Peninsula

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