Journal of Jilin University(Earth Science Edition) ›› 2016, Vol. 46 ›› Issue (1): 146-162.doi: 10.13278/j.cnki.jjuese.201601113

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LA-ICP-MS U-Pb Dating of Detrital Zircons from Linxi Formation and Its Geological Implications in Hexigten Qi, Inner Mongolia

Li Hongying1, Zhang Da1, Zhou Zhiguang1, Liu Changfeng1, Li Pengju2, Chen Lizhen3, Gu Congnan4   

  1. 1. School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China;
    2. School of Economics and Management, Sichuan University of Science & Engineering, Zigong 643000, Sichuan, China;
    3. Regional Geology and Mineral Resources Survey Institute of Hebei, Langfang 065000, Hebei, China;
    4. Tianjin North China Geological Exploration Bureau, Tianjin 300170, China
  • Received:2015-04-25 Online:2016-01-26 Published:2016-01-26
  • Supported by:

    Supported by Mineral Survey Program Issued by Department of Land and Resources of Inner Mongolian Autonomous Region (NMKD2006-05) and Geological Survey Projects of China Geological Survey(1212010811001, 1212011085490, 12120114093901, 1212011220465)

Abstract:

Hexigten Qi is located to the north of Xar Moron River, tectonically on the south margin of Xilinhot massif. The authors conduct the analysis on the detrital zircon LA-ICP-MS U-Pb dating for the metasiltstones of Linxi Formation from a ca. 5 km outcrop in the northeastern Hexigten Qi. The samples yield 4 groups of ages principally at:258-298 Ma (peak at 285 Ma), 377-474 Ma (peak at 430 Ma), 1 261-1 727 Ma, and 1 853-2 513 Ma. Besides, two zircons yield the age of 321 Ma and 937 Ma respectively. Zirons aged 258-298 Ma show oscillatory zones in CL images, reflecting the magmatic events in Late Paleozoic along Xing'an-Mongolia orogenic belt. Zircons with 377-474 Ma ages are featured by both magmatic and metamorphic origins, suggesting that the provenances of Linxi Formation in Hexigten Qi probably were from Ordovician-Devonian magmatic and Paleozoic metamorphic rocks. Zircons yielded ages of 1 261-1 727 Ma are dominated by magmatic zircons, with some metamorphic zircons; indicating that the Mesoproterozoic magmatic and metamorphic rocks are also the provenances of Linxi Formation. Most of the Zircons aged 1 853-2 513 Ma are of magmatic origin, showing the old age information from North China Craton (NCC). The youngest age from this metasiltstone is 258 Ma, which constrains the deposition age of Linxi Formation to Late Permian. The broad scope of ages reflects the tectono-magmatic events both in NCC and Xing'an-Mongolia orogenic belt, and indicates that Linxi Formation has two provenances, and also implies that NCC and Siberia plate had amalgamated before Linxi Formation deposited.

Key words: Linxi Formation, detrital ziron, metusiltstones, U-Pb dating, Hexigten Qi, Xilinhot massif

CLC Number: 

  • P588.3

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