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QU Hongying, LIU Jiannan, PEI Rongfu, HE Shuyue, ZHOU Shumin, WANG Hui, ZHOU Jianhou. 2018. Thermochronology of the monzonitic granite related to the Hutouya Cu-Pb-Zn polymetallic deposit in Qiman Tage, Qinghai Province[J]. Geology in China, 45(3): 511-527. doi: 10.12029/gc20180307
Citation: QU Hongying, LIU Jiannan, PEI Rongfu, HE Shuyue, ZHOU Shumin, WANG Hui, ZHOU Jianhou. 2018. Thermochronology of the monzonitic granite related to the Hutouya Cu-Pb-Zn polymetallic deposit in Qiman Tage, Qinghai Province[J]. Geology in China, 45(3): 511-527. doi: 10.12029/gc20180307
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Thermochronology of the monzonitic granite related to the Hutouya Cu-Pb-Zn polymetallic deposit in Qiman Tage, Qinghai Province

  • 1.

    MLR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China

  • 2.

    No.3 Institute of Geology and Mineral Resources, Xining 810029, Qinghai, China

  • 3.

    Department of Geological Engineering, Qinghai University, Xining 810016, Qinghai, China

    • Fund Project: Supported by China Geological Survey Program(No. DD20160007)
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  • Author Bio: QU Hongying, female, born in 1978, doctor, associate researcher, mainly engages in the study of ore deposition and economic geology; E-mail: hongyingqu@126.com
  • Corresponding author: LIU Jiannan, male, born in 1982, doctor, assistant researcher, mainly engages in the study of ore deposition; E-mail: 454664253@qq.com 
Received Date:  06 July 2017
Revised Date:  12 March 2018
Publish Date:  25 June 2018
    Abstract

  • The Hutouya mining area in Qiman Tage of Qinghai Province owns the characteristics of inner-and exo-contact belt skarn subtype mineralization. The magmatic intrusive activities are strong in this area. The carbonatite formation of different ages is exposed extensively. The combination of metal metallogenic elements is complex. The potential for the ore prospecting is great. This study is based on the thermochronology theory for rock bodies. The total energy of rock bodies is proportional to its scale. The thermal energy is larger as the scale of rock bodies is larger, the thermal effect is larger as the thermal energy is larger, and the cooling rate is larger as the thermal effect is larger. The cooling rate is calculated via the closure temperature of different minerals. The authors studied Ar-Ar ages of biotite and plagioclase from the Hutouya mining area. The 40Ar-39Ar plateau ages of biotite and plagioclase from the HTY002 monzonitic granite sample related to mineralization are 2(33.6 ±2.2) Ma and (231.5 ±1.3) Ma, respectively. The 40Ar-39Ar plateau ages from the HTY016 sample are (229.6±2.3) Ma and (219.3±1.8) Ma, respectively. The 40Ar-39Ar plateau ages of the HTY019 sample are (224.7±2.6) Ma and (222.2±2.2) Ma, respectively. The calculated cooling rates are 57.14℃/Ma, 11.65℃/Ma, and 48.00℃/Ma. Where the compositions of the intrusive rocks are similar, the differences of the unit thermal energies of their emplacement are very small. Because the total energy of rock bodies is proportional to its scale, the total energies of rock bodies of different scales are different. The thermal energy of large rock bodies is large, the time of balance with the surrounding rock is long, the thermal effect is large, and the cooling rate is low. The cooling rates of different minerals from the Hutouya mining area are similar. The values of the cooling rates are high, varying from 11 to 57℃/Ma, so the thermal effect is large. It is thus concluded that the potential for the ore prospecting is great in the Hutouya mining area.

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