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2021 Vol. 48, No. 5
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LIU Fang, WANG Xi, HAI Lianfu, ZHAO Dongsheng. 2021. Zircon U-Pb ages, Hf isotope and extensional tectonics of monzogranite in the Hansumu area of southern Great Khingan[J]. Geology in China, 48(5): 1609-1622. doi: 10.12029/gc20210521
Citation: LIU Fang, WANG Xi, HAI Lianfu, ZHAO Dongsheng. 2021. Zircon U-Pb ages, Hf isotope and extensional tectonics of monzogranite in the Hansumu area of southern Great Khingan[J]. Geology in China, 48(5): 1609-1622. doi: 10.12029/gc20210521
shu

Zircon U-Pb ages, Hf isotope and extensional tectonics of monzogranite in the Hansumu area of southern Great Khingan

  • 1.

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

  • 2.

    Geological Bureau of Ningxia Hui Autonomous Region, Yinchuan 750021, Ningxia, China

  • 3.

    College of Earth Sciences, Jilin University, Changchun 130012, China

  • 4.

    Ningxia Mineral and Geological Survey Institute, Yinchuan 750021, Ningxia, China

  • 5.

    Chifeng Institute of Geological and Mineral Exploration and Development, Inner Mongolia, Chifeng 024000, Inner Mongolia, China

    • Fund Project: Supported by the project of China Geological Survey(No.DD20160048, No.12120115031701)and innovation team of geological and mineral resources exploration and development in Ningxia(No.201605)
More Information
  • Author Bio: LIU fang, born in 1981, female, senior engineer, doctor candidate, engaged in magmatic activities, mineral geological prospecting and research; E-mail: 834414859@qq.com
Received Date:  06 May 2019
Revised Date:  16 December 2019
Publish Date:  25 October 2021
    Abstract

  • Large area of monzogranite is outcropped in the Hansumu area of southern Great Khingan. In order to recognize the formation age of the rock and its tectonic significance, samples were collected from the monzogranite pluton to study its petrography, zircon LA-MC-ICP-MS age and Hf isotope. The results show that the pluton is composed of fine-grained porphyritic amphibolit-biotite monzogranite and fine-grained porphyritic biotite monzogranite with porphyritic and porphyritic structures and massive structures. The zircons from the monzogranite is of magmatic origin, and yields 206Pb/238U age of 136±1 Ma (MSWD=1.4), which suggests that the pluton was formed in the late Early Cretaceous. This result is strongly consistent with the study area and its surrounding areas, and even with the 114-145 Ma magmatic activities in the northeastern of China, indicating the products of the same magmatic activity stage. The monzogranite in the Hansumu area has positive εHf (t) values of 7.1 to 14.4 and young Hf two-stage model ages, and TDM2 is 324 to 959 Ma. Young Hf isotope model ages imply that this area could have experienced an important crustal accretion event during the Neoproterozoic-Late Proterozoic. Combined with regional geology, it is suggested that the monzogranite was likely derived from the partial melting of young mantle, and possibly was formed in a lithosphere extensional tectonics environment related to the subduction of the Paleo-Asian plate to Eurasia Plate.

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