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SHEN Liang, ZHAO Shengjin, YU Haiyang, LIU Zhihui, ZHOU Yingshuai, ZHANG Meng, PIAO Lili. 2020. Zircon age and geochemical characteristics of Hadataolegai Formation volcanic rocks in Da Hinggan Mountains and its continental marginal arc setting[J]. Geology in China, 47(4): 1041-1055. doi: 10.12029/gc20200410
Citation: SHEN Liang, ZHAO Shengjin, YU Haiyang, LIU Zhihui, ZHOU Yingshuai, ZHANG Meng, PIAO Lili. 2020. Zircon age and geochemical characteristics of Hadataolegai Formation volcanic rocks in Da Hinggan Mountains and its continental marginal arc setting[J]. Geology in China, 47(4): 1041-1055. doi: 10.12029/gc20200410
shu

Zircon age and geochemical characteristics of Hadataolegai Formation volcanic rocks in Da Hinggan Mountains and its continental marginal arc setting

  • 1.

    Development and Research Center of China Geological Survey, Beijing 100037, China

  • 2.

    No. 10 Institute of Geological Exploration, Inner Mongolia Bureau of Geology and Mineral Resources, Chifeng 024005, Inner Mongolia, China

  • 3.

    Inner Mogolia Tenth Geological Mineral Exploration and Development Co., Ltd., Chifeng 024005, Inner Mongolia

  • 4.

    School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China

    • Fund Project: Supported by China Geological Survey Projects (No.DD20160048- 15, 12120114086201, DD20190405 and DD20190406)
More Information
  • Author Bio: SHEN Liang, female, born in 1983, doctor, engineer, majors in regional geology research; E-mail:2547163401@qq.com
  • Corresponding author: ZHAO Shengjin，male，born in 1982，doctor，senior engineer, majors in mineralogy, petrology ans mineral deposits, engages in regional survey of geology and mineral resources；E-mail：zhshjin2008@163.com 
Received Date:  12 October 2019
Revised Date:  18 June 2020
Publish Date:  25 August 2020
    Abstract

  • A series of volcanic rocks, such as basalt, andesite and rhyolite, were determined in Xin Barag Right Banner of northern Da Hinggan Mountains. Geological survey reveals that these volcanic rocks should be assigned to Hadataolegai Formation. SHRIMP zircon U-Pb dating indicates that the epidotized andesite from Hadataolegai Formation was formed at(254.3±7.9)Ma(MSWD=4.7). According to geochemical researches, these volcanic rocks of Hadataolegai Formation can be divided into two types, i.e., intermediate-basic rocks and acidic rocks. The magma of intermediate-basic rocks was derived from the lithospheric mantle affected by the southward subduction of Mongolia-Okhotsk plate. The acidic volcanic rocks have a crustal-derived magma source features. Based on tectonic setting analysis, the authors hold that the Hadataolegai Formation volcanic rocks were formed under the continental marginal arc environment and related to southward subduction of Mongolia-Okhotsk plate. The determination of Hadataolgegai Formation improves the stratigraphic sequence of northern Da Hinggan Mountains and provides a favorable evidence for regional tectonic evolution of Da Hinggan Mountains.

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