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Home » Uprising period and elevation of the Wenyu granitic pluton in Xiaoqinling District, Central China

  1. Uprising period and elevation of the Wenyu granitic pluton in Xiaoqinling District, Central China

    Author Name: XinQi Yu, JunLai Liu, DeHui Zhang, Yong Zheng, ChunLin Li

    Xiaoqinling District is an important gold-producing area in China. It ranks second to Jiaodong with regard to gold deposits. The uprising period of the Wenyu granitic pluton and the wall-rocks of the deposit, as well as the mineralizing depth and reserved place of gold ore bodies, are significant to ore exploration. Fission-track (FT) analysis of zircons and apatites of granitic rocks from the Wenyu granitic pluton shows that apatite FT (AFT) data modeling indicates a rapid cooling rate of 20°C/Ma from 138 to 120 Ma after emplacement at 138 Ma. Thermal evolution and inversion curves suggest a secondary phase of fast cooling and uprising from 45 to 35 Ma, and 35 Ma, respectively, with a cooling rate of 6.7°C/Ma and a denudation quantity of

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