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    中国百强科技报刊

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    Volume 37 Issue 1
    Jan.  2012
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    Article Navigation >  Earth Science  > 2012  >  37(1): 125-138
    HUANG Hu, YANG Jiang-hai, DU Yuan-sheng, HUANG Hong-wei, HUANG Zhi-qiang, XIE Chun-xia, Hu Li-sha, 2012. LA-ICPMS U-Pb Dating of Zircons from Tuffs of the Upper Permian-Middle Triassic in Youjiang Basin, Guangxi Province and Its Geological Significance. Earth Science, 37(1): 125-138. doi: 10.3799/dqkx.2012.012
    Citation: HUANG Hu, YANG Jiang-hai, DU Yuan-sheng, HUANG Hong-wei, HUANG Zhi-qiang, XIE Chun-xia, Hu Li-sha, 2012. LA-ICPMS U-Pb Dating of Zircons from Tuffs of the Upper Permian-Middle Triassic in Youjiang Basin, Guangxi Province and Its Geological Significance. Earth Science, 37(1): 125-138. doi: 10.3799/dqkx.2012.012
    shu

    LA-ICPMS U-Pb Dating of Zircons from Tuffs of the Upper Permian-Middle Triassic in Youjiang Basin, Guangxi Province and Its Geological Significance

    doi: 10.3799/dqkx.2012.012
    • 1.

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

    • 2.

      General Academy of Geological Survey of Guangxi, Nanning 530023, China

    • Received Date: 2010-07-05
    • Publish Date: 2012-01-15
      Abstract
    • Upper Permian-Middle Triassic sections in Youjiang basin contain many volcanic tuff horizons. Zircon LA-ICP-MS U-Pb dating of 4 volcanic tuff samples from the bottom of the Luolou and Baifeng formations in the Jiuxu and Lizhou areas, Guangxi Province, yield the depositional ages of 252.8±1.8, 253.0±2.4, 247.2±1.5 and 239.3±2.7 Ma, respectively, which, together with the inherited or xenocrystal zircon ages (with peak values of 264 and 267 Ma), indicate that episodical volcanism occurred during Middle Permian Gudalupian and Middle Triassic Bithynian in southwestern China. The appearance of the inherited zircon ages (260~270 Ma) from the volcanic tuffs around the Permian-Triassic boundary (PTB) indicate the volcanic events in South China may have caused the End-Permian extinction. The depositional age of 247.2±1.5 Ma from the volcanic tuff at the bottom of the Middle Triassic Baifeng Formation indicates it is more appropriate to place the Early to Middle Trissic boundary at 247.2 Ma. The petrographical study of the volcanic tuffs indicates the Youjiang basin expierenced the tectonic transition from extension to compression after Middle Triassic, and especially after Bithynian, which resulted in the great tectonic subsidence of the basin.

       

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