Welcome to visit Geoscience!

Geoscience ›› 2022, Vol. 36 ›› Issue (01): 282-294.DOI: 10.19657/j.geoscience.1000-8527.2021.046

• Petrology • Previous Articles     Next Articles

Zircon U-Pb Geochronology, Hf isotope and Whole-Rock Geochemical Characteristics of Xiaohanshan Pluton in Haobugao Pb-Zn Deposit, Inner Mongolia

ZHU Tong1,2,3(), SUN Zhenjun1,2(), YU Henan1,2, WANG Chengyang1,2, LIU Guanghu1,2   

  1. 1. School of Earth Science, China Institute of Disaster Prevention, Sanhe, Hebei 101601, China
    2. Hebei Key Laboratory of Earthquake Dynamics, Sanhe, Hebei 101601, China
    3. College of Earth Science, Guilin University of Technology, Guilin, Guangxi 541004, China
  • Received:2020-11-20 Revised:2021-11-10 Online:2022-02-10 Published:2022-03-08
  • Contact: SUN Zhenjun

Abstract:

The Haobugao lead-zinc deposit is tectonically located in the southern part of the Great Xing’an Range, and is part of the Huanggangliang-Ganzhuermiao tectono-metallogenic belt. In this paper, detailed data on petrology, U-Pb geochronology, geochemistry and Hf isotopes were presented on the Xiaohanshan pluton of the Haobugao lead-zinc deposit. The results show that the main rock type of the Xiaohanshan pluton is monzogranite, which was formed in the Early Cretaceous (143.9±1.1 Ma). The rocks have high SiO2 (66.96%-68.05%) and alkali (Na2O+K2O=9.91%-10.09%), but low Al2O3 (15.69%-16.49%), CaO (1.22%-1.41%), and TFe2O3/MgO (average 8.29). The rocks belong to metaluminous to peraluminous granites with right-inclining REE distribution patterns and distinct negative Eu anomalies (0.33-0.41). The samples also show enrichments in large ion lithophilic elements (LILEs, e.g., Rb, K) and other incompatible elements (e.g., Th, U), whereas high field strength elements (HFSEs, e.g., Nb, P, Nb, Ta, Ti) are depleted, showing A2-type granite affinity. The rocks have initial 176Hf/177Hf values of 0.282,829-0.282,936(average 0.282,888) and εHf(t) of 4.4 to 8.4 (average 6.7), indicating that the Xiaohanshan pluton is mainly derived from partial melting of the middle and lower crust with minor mantle material input. It is considered that formation of the Xiaohanshan pluton was related to the post-collision extensional tectonics in the Early Cretaceous Paleo-Pacific subduction continental margin.

Key words: geochemistry, zircon U-Pb dating, Early Cretaceous, Xiaohanshan pluton, Haobugao lead-zinc deposit

CLC Number: