Hydrothermal Zircon Geochronology in the Shangxu Gold Deposit and its Implication for the Early Cretaceous Orogenic Gold Mineralization in the Middle Bangonghu–Nujiang Suture Zone,Acta Geologica Sinica-English Edition

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Hydrothermal Zircon Geochronology in the Shangxu Gold Deposit and its Implication for the Early Cretaceous Orogenic Gold Mineralization in the Middle Bangonghu–Nujiang Suture Zone
Acta Geologica Sinica-English Edition ( IF 3.3 ) Pub Date : 2021-03-24 , DOI: 10.1111/1755-6724.14679
Hanxiao HUANG ₁ , Jiancuo LUOSANG ₂ , Zuowen DAI ₃ , Hong LIU _{1,

4} , Jiangang FU ₁ , Guangming LI ₁ , Huawen CAO ₁ , Qing ZHOU ₁

Affiliation

As a typical orogenic gold deposit in Tibet, Shangxu gold deposit is located at the Bangong Lake–Nujiang River Metallogenic Belt in the south of Qinghai–Tibet Plateau. In this paper, zircon U-Pb dating, trace elements and Hf isotopic analysis were performed on Au-bearing quartz veins in the Shangxu gold deposit. Zircons from Au-bearing quartz veins can be divided into three types: detrital, magmatic, and hydrothermal zircons. There are two age peaks in detrital zircons: ca. 1700 Ma and ca. 2400 Ma. There are two groups of concordant ages including 157 ± 4 Ma (MSWD = 0.69) and 120 ± 1 Ma (MSWD = 0.19) in magmatic zircons, in which ε_Hf(t) value of ca. 120 Ma from the magmatic zircons range from +8.24 to +12.9. An age of 119 ± 2 Ma (MSWD = 0.42) was yielded from hydrothermal zircons, and their ε_Hf(t) values vary between +15.7 and +16.4. According to sericite Ar-Ar age, this paper suggests that an age of 119 ± 2 Ma from hydrothermal zircons represent the formation age of the Shangxu gold Deposit, and its mineralization should be related to the collision between Lhasa Block and Qiangtang Block. The metallogenic age is basically the same as the diagenetic age of Mugagangri granite, and ε_Hf(t) value of hydrothermal zircon is significantly higher than that of the contemporaneous magmatic zircon, which indicates that there is a genetic relationship between the gold mineralization and the deep crust-mantle magmatism.

更新日期：2021-03-24

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