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Shanxi Provincial Education Department
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Taiyuan University of Technology
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Ed. Office of Journal of TYUT
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SUN Hongbin
ISSN: 1007-9432
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  • Geochronology Definition of Jian'ancun Formation in Wutai Hutuo Group and Its Implications
    DOI:
    10.16355/j.tyut.1007-9432.20230507
    Received:
    Accepted:
    abstract:
    PurposesThe Hutuo Group belongs to the Early Proterozoic strata. As one of the most typical Paleoproterozoic strata in North Chinathe timing redefinition of the Hutuo Group is of great significance to the establishment of the earlyPrecambrian stratigraphic chronology frameworkthe discussion of the early Precambrian geological evolution process in North China and the study of plate assembly.MethodsThis article conducts a detailed study of the Dongye Subgroup strata of the Hutuo Groupcollecting 24 detrital zircon samples from the Jian'ancun Formation of the Hutuo Group. From 23 similar age detrital zirconswe define the weighted average age of the bottom boundary of the Hutuo Group is 2 469 Maand regional tectonic movements occurred in the Wutai area around 1 855 Ma. According to the 1 109 zircon ages in Hutuo Group from previous studieswe considered that the ages of >2.5 Ga are from underlying Gaofan subgroup and the maximum depositional age of Hutuo Group was early Paleoproterozoic.FindingsThe results show that the crust of the Wutai area was unstable at 2 3762 1702 0661 988and 1 825 Maresulting in multiple magmatic events. The 1 825 Ma zircon age can further indicate the occurrence of the Lyuliang movementand provide a basis for the early Proterozoic North China Craton integration.
    Keywords:
    wutai mountain; Jian'ancun formation; zircon U-Pb dating; Hutuo group; early paleoproterozoic;

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