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Volume 39 Issue 6
Nov.  2020
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Article Navigation >  Bulletin of Geological Science and Technology  > 2020  >  39(6): 64-74
Zhao Yanyan, Tan Jun, Liu Xiaoyang, Zhang Ming, Chen Yang, He Di. Inclusion features and geological significance of the Tonglüshan skarn-type copper-iron (gold) deposit in Daye, Hubei[J]. Bulletin of Geological Science and Technology, 2020, 39(6): 64-74. doi: 10.19509/j.cnki.dzkq.2020.0606
Citation: Zhao Yanyan, Tan Jun, Liu Xiaoyang, Zhang Ming, Chen Yang, He Di. Inclusion features and geological significance of the Tonglüshan skarn-type copper-iron (gold) deposit in Daye, Hubei[J]. Bulletin of Geological Science and Technology, 2020, 39(6): 64-74. doi: 10.19509/j.cnki.dzkq.2020.0606
shu

Inclusion features and geological significance of the Tonglüshan skarn-type copper-iron (gold) deposit in Daye, Hubei

doi: 10.19509/j.cnki.dzkq.2020.0606
  • Received Date: 20 Sep 2019
    Abstract
  • The Tonglüshan copper-iron (gold) deposit is a typical skarn deposit in the middle and lower reaches of the Yangtze River in Hubei.In order to find the origin of skarn, the petrographic observation, microscopic temperature measurement and laser Raman analysis of the inclusions were carried out.The result shows that the uniform temperature of the fluid inclusions in the deposit ranges from 180 to 700℃, and the salinity ranges from 1.74% to 55.7% NaCleqv. From the skarn period to the quartz-sulfide period, the ore-forming fluids are from high temperature and high salinity to low temperature and low salinity.The result of laser Raman measurement shows that the melt inclusions contain garnet, calcite, hematite and water.Based on the petrography and petrofacies composition characteristics of inclusions, the early skarn of Tonglüshan deposit should be of magmatic origin.

     

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