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QIN Xuping, LI Dewei, LIU Jianxiong, MAO Chen. 2018. Yanshanian thermo-upwelling extension and palaeo-hydrothermal system in southeast Guangdong: A case study of Enping-Xinfeng detachment fault[J]. Geology in China, 45(6): 1188-1204. doi: 10.12029/gc20180609
Citation: QIN Xuping, LI Dewei, LIU Jianxiong, MAO Chen. 2018. Yanshanian thermo-upwelling extension and palaeo-hydrothermal system in southeast Guangdong: A case study of Enping-Xinfeng detachment fault[J]. Geology in China, 45(6): 1188-1204. doi: 10.12029/gc20180609
shu

Yanshanian thermo-upwelling extension and palaeo-hydrothermal system in southeast Guangdong: A case study of Enping-Xinfeng detachment fault

  • 1.

    Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, Hubei, China

  • 2.

    China Nonferrous Metals(Guilin) Geology and Mining Co, . Ltd, Guilin 541000, Guangxi, China

  • 3.

    Foshan Geological Bureau of Guangdong Province, Foshan 528000, Guangdong, China

  • 4.

    Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, Hubei, China

    • Fund Project: Supported by China Geological Survey Program (No. 1212011121246, 1212011220400) and National Natural Science Foundation of China (No. 41172188)
More Information
  • Author Bio: QIN Xuping, male, born in 1991, master candidate, engages in the study of regional thermal controlling structures and geothermal systems; E−mail: 1459315842@qq.com
  • Corresponding author: LI Dewei, male, born in 1962, supervisor of doctor candidates, engages in the study of structure geology, tectonics and their applications in energy and disasters; E−mail: dewei89@sina.com 
Received Date:  16 April 2016
Revised Date:  06 August 2017
Publish Date:  25 December 2018
    Abstract

  • NE-SW trending Yanshanian detachment faults are widely spread in southeast Guangdong. The authors carried out geological survey and physical and chemical test of Enping-Xinfeng detachment fault, with emphasis placed on the mylonite in the ductile shear zone below this detachment fault and the silicified rocks related to the high angle normal fault on the hanging wall of the detachment fault. The authors believe that the initiation age of the upwelling-extension structure was in early Yanshanian, the deformation temperatures of the mylonite which had the kinematic property of ductile rheology in the ductile shear zone were about 350℃, and the mylonite was brought onto the surface during later tectonic uplift. The microthermometric study of the fluid inclusions in the silicified rocks indicates that the homogeneous temperatures of the fluid inclusions are between 155℃ and 326℃. The salinities are between 2.74% and 21.61% NaCleqv, with an average of 11.17% NaCleqv, the temperatures of the silicon-contained hot liquid are about 241℃, and the silicon-contained hot liquid is believed to be NaCl-H2O solution with rich silicon and carbon dioxide according to Laser-Raman microspectroscopy. Compositions of H-O stable isotope imply that the paleo-hydrothermal fluids were derived from the mixing of magmatic water and rain water in the study area. The silicified rocks distributed along the strike of the normal fault possibly are the significant indications of the paleo-hydrothermal system in Yanshanian. The thermo-upwelling extension system and the deep and shallow integrated palaeo-hydrothermal system in the late Yanshanian are significant for the understanding of the type, the mechanism and the distribution regularities of the modern geothermal system in southeast Guangdong.

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