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2020 Vol. 47, No. 4
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Article navigation > Geology in China > 2020 > 47(4): 985-997
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WANG Xiaohu, ZHANG Wengao, CHEN Zhengle, ZHOU Rongde, CHEN Bailin, XU Diankui, HUO Hailong, LI Jilin, ZHANG Tao, DING Zhilei, LI Xiaozhuang. 2020. Deformation time limit of ore-controlling structures in Lianhuashan fault zone along the South China coast:Constraints from zircon U-Pb age and stratigraphic age[J]. Geology in China, 47(4): 985-997. doi: 10.12029/gc20200406
Citation: WANG Xiaohu, ZHANG Wengao, CHEN Zhengle, ZHOU Rongde, CHEN Bailin, XU Diankui, HUO Hailong, LI Jilin, ZHANG Tao, DING Zhilei, LI Xiaozhuang. 2020. Deformation time limit of ore-controlling structures in Lianhuashan fault zone along the South China coast:Constraints from zircon U-Pb age and stratigraphic age[J]. Geology in China, 47(4): 985-997. doi: 10.12029/gc20200406
shu

Deformation time limit of ore-controlling structures in Lianhuashan fault zone along the South China coast:Constraints from zircon U-Pb age and stratigraphic age

  • 1.

    Laboratory of Dynamic Diagenesis and Metallogenesis, Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China

  • 2.

    No. 931 Geological Party, Nonferrous Metals Geological Bureau of Guangdong Province, Shantou 515041, Guangdong, China

    • Fund Project: Supported by China Geological Survey Projects (No. DD20160053, No. DD20190161)and the projects of Basic Scientific Research Fund(No. YYWF201614, Academy and Institute Dean Foundation 46)
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  • Author Bio: WANG Xiaohu, male, born in 1983, doctor, associate researcher, supervisor of master candidates, engages in the study of mineral deposits and structural ore-controlling role; Email:wangzykc@yeah.net
Received Date:  18 September 2019
Revised Date:  07 November 2019
Publish Date:  25 August 2020
    Abstract

  • The Lianhuashan fault zone is not only an important NE-striking fault zone in Guangdong Province but also a significant tin, tungsten, copper, lead-zinc polymetallic metallogenic belt. Based on geological field observation of the Lianhuashan fault zone and the typical mining area as well as the measurement of the zircon U-Pb age of the granite intrusive with ductile deformation, the authors preliminarily investigated the time of ductile deformation and boundary fault and the relationship between deformation and mineralization in this paper. The result indicates that the ductile deformation time in the Lianhuashan fault zone is around 129-127 Ma, and the brittle boundary fault was developed between the sedimentary time of Guancaohu Formation and the Heshui Formation. The age of ductile shear deformation in the Lianhuashan fault zone was earlier than the mineralization time, and the ductile shear deformation provided the ore-bearing space for mineralization.

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