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JIANG Haoyuan, ZHAO Zhidan, ZHU Xinyou, YANG Shangsong, JIANG Binbin, YANG Chaolei, MAO Chunwei. 2020. Characteristics and metallogenic significance of granite porphyry and pyroxene diorite in the Bianjiadayuan Pb-Zn-Ag polymetallic deposit, Inner Mongolia[J]. Geology in China, 47(2): 450-471. doi: 10.12029/gc20200213
Citation: JIANG Haoyuan, ZHAO Zhidan, ZHU Xinyou, YANG Shangsong, JIANG Binbin, YANG Chaolei, MAO Chunwei. 2020. Characteristics and metallogenic significance of granite porphyry and pyroxene diorite in the Bianjiadayuan Pb-Zn-Ag polymetallic deposit, Inner Mongolia[J]. Geology in China, 47(2): 450-471. doi: 10.12029/gc20200213
shu

Characteristics and metallogenic significance of granite porphyry and pyroxene diorite in the Bianjiadayuan Pb-Zn-Ag polymetallic deposit, Inner Mongolia

  • 1.

    Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, Gansu, China

  • 2.

    Key Laboratory of Petroleum Resources, Gansu Province/Key Laboratory of Petroleum Resources Research, Institute of Gelogy and Geophysics, Chinese Academy of Sciences, Lanzhou 730000, Gansu, China

  • 3.

    University of Chinese Academy of Sciences, Beijing 100049 China

  • 4.

    Beijing Institute of Geology for Mineral Resources, Beijing 100012, China

  • 5.

    China University of Geosciences(Beijing), Beijing 100083, China

    • Fund Project: Supported by China National Geological Survey National Secondary Project Inner Mongolia Chifeng Nonferrous Metals Base Comprehensive Geological Survey (No. DD20160072) and National Natural Science Fund (No. 41602098)
More Information
  • Author Bio: JIANG Haoyuan, male, born in 1995, doctor candidate, mainly engages in the study of geochemistry; Email:janghaoyuan@outlook.com
  • Corresponding author: ZHU Xinyou, male, born in 1965, doctor, engages in the study of mineral deposits; E- mail:zhuxinyou@outlook.com 
Received Date:  21 July 2018
Revised Date:  10 October 2019
Publish Date:  25 April 2020
    Abstract

  • Located in the southern section of the CAOB (Central Asian Orogenic Belt), the Bianjiadayuan Pb-Zn-Ag polymetallic deposit belongs to the Sn-Cu-Zn-Pb metallogenic belt of Da Hinggan Mountains. In this study, a series of analyses, such as LAICP-MS zircon U-Pb isotopic dating, major element and trace elements testing and electron microprobe analysis of albite, were performed for the granite porphyry and augite diorite. The results show that the age of granite porphyry and pyroxene diorite are ca. 138 Ma and ca.137 Ma respectively, indicating that the intrusive rocks are products of the magmatic activities in the Early Cretaceous. The pyroxene diorite belongs to high K calc-alkaline series and calc-alkaline series with SiO2 (50.99%-52.89%), CaO (7.4%7-7.51%), MgO (3.64%-4.68%), and alkali (Na2O+K2O) 4.91%-5.36%. Granitic porphyry with miarolitic structure and microscopic identification shows that feldspar is all alkaline feldspar. Non-mineralized granite porphyry is characterized by high SiO2 (50.99%-52.89%), alkali (Na2O+K2O=4.83%-9.42%), A/CNK (1.13-2.40), LREE enrichment, strong negative Eu anomalies (δEu=0.12-0.32), enrichment of LILE such as Rb, Th, U and K, depletion of HFSE such as Ta, Nb, P and Ti and transition elements such as Sr and Ba. According to the electron microprobe analyses, the An values of the albite in granite porphyry are by far lower than 10 (0.03-4.64). These features are similar to the features of typical highly evolved A2 post-orogenic alkali feldspar granite pluton, suggesting that the magma was derived from the lithospheric mantle and formed in the tensional setting. Combined with the geological characteristics and previous research results, the authors hold hat the metallogenic geological body of the Bianjiadayuan area is the granite porphyry pluton, and there is still a great potential for mineralization in the deep part of western mining area.

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