Volume 43 Issue 12
Dec.  2018
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Article Navigation >  Earth Science  > 2018  >  43(12): 4551-4565
Zhao Yayun, Liu Xiaofeng, Liu Yuanchao, Ci Qiong, Xiao Lanbin, Li Li, Zhang Xiaoqiang, 2018. Zircon U-Pb Ages and Geochemical Characteristics of Youqiumi Porphyry Pluton in Cimabanshuo Area, Tibet. Earth Science, 43(12): 4551-4565. doi: 10.3799/dqkx.2018.118
Citation: Zhao Yayun, Liu Xiaofeng, Liu Yuanchao, Ci Qiong, Xiao Lanbin, Li Li, Zhang Xiaoqiang, 2018. Zircon U-Pb Ages and Geochemical Characteristics of Youqiumi Porphyry Pluton in Cimabanshuo Area, Tibet. Earth Science, 43(12): 4551-4565. doi: 10.3799/dqkx.2018.118
shu

Zircon U-Pb Ages and Geochemical Characteristics of Youqiumi Porphyry Pluton in Cimabanshuo Area, Tibet

doi: 10.3799/dqkx.2018.118
  • 1.

    No.2 Geological Team, Tibet Autonomous Region Geological Mining Exploration and Development Bureau, Lhasa 850003, China

  • 2.

    Tibet Autonomous Region Geological Mining Exploration and Development Bureau, Lhasa 850000, China

  • 3.

    No.7 Geological Team, Non-Ferrous Metals and Nuclear Industry Geological Exploration Bureau of Guizhou, Guiyang 550005, China

  • Received Date: 2018-05-05
  • Publish Date: 2018-12-15
    Abstract
  • The ore-bearing porphyry body has favorable geological conditions for porphyry copper mineralization in Cimabanshuo area, Tibet. Therefore, it is of great significance to study the geological background and genesis of diagenesis and mineralization in this area. In this paper, combined with their new understanding and new discoveries in the field works, the authors carried out a detailed research of zircon U-Pb dating and petrogeochemistry, for Youqiumi pluton in Cimabanshuo area.The results show that the granodiorite-poryphy yields an LA-ICP-MS zircon U-Pb age of 15.2±0.8 Ma to 15.2±0.7 Ma, namely the formation age of Miocene. Chemical analyses show that the granodiorite-poryphy has a characteristic of high SiO2 (65.08%-66.85%), high K2O (3.85%-4.58%), rich K2O+Na2O (7.87%-8.90%), depleted MgO (1.51%-1.84%), meta-aluminum (A/CNK=0.88-0.95). Chondrite-normalized REE distribution pattern diagrams display right-incline and weakly negative Eu anomalies, differentiated obviously (La/Yb)N=36.60-47.43. Enriched strongly in compatible elements such as Rb, Th, U, K and depleted in high field strength elements (HFSEs) such as Nb, Ta, Ce, P, Ti. Specifically, Youqiumi granitic pluton shows typical adakitic signatures:high Sr (674×10-6 to 876×10-6) and low Yb (0.560×10-6 to 0.757×10-6) and low Y (7.97×10-6 to 9.98×10-6), contents with high Sr/Y ratios (73.84-109.98). However, the whole-rock Sr, Nd isotopic compositions of granodiorite-poryphy have initial 87Sr/86Sr ratios and εNd(t) values are 0.707 878 and -8.26 respectively, with ancient Nd two-phase model ages of 1 503 Ma, which indicate that the magma sources may have contributed to partial melting of previous juvenile lower crust.Combined with igneous rocks in the studied area, it is proposed that Youqiumi granitic pluton was formed in post-collisional extension setting of India-Asia contional collision orogenic belt.

     

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