Volume 47 Issue 8
Sep.  2022
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Article Navigation >  Earth Science  > 2022  >  47(8): 2925-2939
Gao Qiuling, Chen Zhong-Qiang, Zhang Ning, Xia Xuefei, Jiang Tengfei, Wang Guoqing, Xiao Ming, Chen Qing, 2022. Felsic Volcanisms across the Wuchiapingian⁃Changhsingian Boundary (Late Permian) in the Dawoling Section, Jiahe Area, Hunan Province. Earth Science, 47(8): 2925-2939. doi: 10.3799/dqkx.2022.175
Citation: Gao Qiuling, Chen Zhong-Qiang, Zhang Ning, Xia Xuefei, Jiang Tengfei, Wang Guoqing, Xiao Ming, Chen Qing, 2022. Felsic Volcanisms across the Wuchiapingian⁃Changhsingian Boundary (Late Permian) in the Dawoling Section, Jiahe Area, Hunan Province. Earth Science, 47(8): 2925-2939. doi: 10.3799/dqkx.2022.175
shu

Felsic Volcanisms across the Wuchiapingian⁃Changhsingian Boundary (Late Permian) in the Dawoling Section, Jiahe Area, Hunan Province

doi: 10.3799/dqkx.2022.175
  • 1.

    School of Environmental and Biological Engineering, Henan University of Engineering, Zhengzhou 451191, China

  • 2.

    Faculty of Earth Science, China University of Geosciences, Wuhan 430074, China

  • 3.

    State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430074, China

  • 4.

    Jianghan Oilfield Company, SINOPEC, Qianjiang 433124, China

  • 5.

    Shandong Lunan Institute of Geo-Engineering Exploration, Jining 272100, China

  • Received Date: 2022-04-08
  • Publish Date: 2022-09-25
    Abstract
  • The volcanisms of the Guadalupian⁃Lopingian (also middle⁃late Permian) and Permian⁃Triassic boundaries in South China have attracted increasing attentions from geologists. In contrast, less studies concerned the volcanisms between the two. Here, we report geochemical studies on volcanisms near the Wuchiapingian ⁃ Changhsingian boundary within the late Permian from the Dawoling section of Jiahe Area, Hunan Province, South China, in which three layers of claystones, named as HD08, HD12 and HD20, are pronounced in the Wuchiapingian⁃Changhsingian boundary beds that are calibrated to the lower and middle Dalong Formation. The integrated analyses of whole⁃rock geochemistry, zircon U⁃Pb chronology, trace elements and Lu⁃Hf isotopes reveal that these three claystones originated from altered volcanic ashes, representing three episodes volcanism across the Wuchiapingian⁃Changhsingian boundary. The whole⁃rock and zircon trace element signatures indicate that the volcanic ashes originated from rhyolitic or rhyodacitic volcanism, with calc⁃alkaline affinities, and formed in post⁃collisional tectonic settings in the convergent continental margins. Among them, εHf(t) values of HD08 and HD20 are -6.4 to 7.1, with a wide range of variability, and the magma originates from the mixing of Emeishan/Neoproterozoic neogenic crustal materials of and ancient crustal materials; εHf(t) values of HD12 are -12.0 to -3.5, and the magma mainly originates from ancient crustal materials. These three volcanic ash layers, together with previous researches, further confirm the occurrence of intense felsic volcanisms related to the convergence of the Pangea supercontinent in the areas around the South China block during the middle of the Lopingian (late Permian).

     

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