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WANG Xianguang, HU Zhenghua, HUANG Qiuyun, YI Wei, CHEN Guohua, HU Langming, YOU Wei. Zircon U-Pb age of ore-forming magmatic rocks in the Tongjiangling coppertungsten deposit in the Jiurui ore concentration area and its significance[J]. GEOLOGY IN CHINA, 2019, 46(4): 832-840. DOI: 10.12029/gc20190413
Citation: WANG Xianguang, HU Zhenghua, HUANG Qiuyun, YI Wei, CHEN Guohua, HU Langming, YOU Wei. Zircon U-Pb age of ore-forming magmatic rocks in the Tongjiangling coppertungsten deposit in the Jiurui ore concentration area and its significance[J]. GEOLOGY IN CHINA, 2019, 46(4): 832-840. DOI: 10.12029/gc20190413

Zircon U-Pb age of ore-forming magmatic rocks in the Tongjiangling coppertungsten deposit in the Jiurui ore concentration area and its significance

Funds: 

China Geological Survey Program DD20160082

China Geological Survey Program DD20190012

the Geological Prospecting Fund of Jiangxi Province 20160037

More Information
  • Author Bio:

    WANG Xianguang, male, born in 1962, senior engineer, mainly engages in mineral exploration and management; E-mail:1138066942@qq.com

  • Corresponding author:

    HU Zhenghua, male, born in 1985, engineer, mainly engages in mineral exploration and management; E-mail:hucdut@qq.com

  • Received Date: April 19, 2019
  • Revised Date: July 08, 2019
  • Available Online: September 25, 2023
  • The orebodies in the Tongjiangling copper-tungsten mining area generally strike northeast and dip southeast, and occur as layers and lenses near the contact zone between the granodiorite porphyry and carbonate of the Maokou Formation. The ore minerals are mainly composed of chalcopyrite and scheelite. The metallogenic magmatic rocks in this area are granodiorite porphyry with zircon U-Pb age of (143.31+0.62) Ma. Mineralization zoning in the Tongjiangling mining area is characterized by "copper in the upper part and copper and tungsten in the lower part". The contact zone between Carboniferous and Ordovician carbonate rocks and granodiorite porphyry or the Wutong plane and the silica-calcium interface formed during Ordovician-Silurian in the mining area have a great potential for tungsten exploration.

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