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Geoscience ›› 2020, Vol. 34 ›› Issue (05): 1028-1042.DOI: 10.19657/j.geoscience.1000-8527.2020.042

• Petrology • Previous Articles     Next Articles

Volcanic Characteristics, LA-ICP-MS Zircon U-Pb Ages of Claystone at the Permian-Triassic Boundary, Guanba Area in Guizhou Province, South China and the Geological Implications

HE Bi1(), ZHANG Xiangwen1, ZHAO Fei1, JIN Canhai2, REN Guangming2, WANG Ningzu1, ZHANG Wenbin1, ZHANG Zhixi1, SUN Pingyuan1   

  1. 1. The Second Institute of Geology and Minerals Exploration Team,Gansu Provincial Bureau of Geology and Minerals Exploration and Development,Lanzhou,Gansu 730020,China
    2. Chengdu Center,China Geological Survey,Chengdu,Sichuan 610081,China
  • Received:2018-09-12 Revised:2020-06-16 Online:2020-10-28 Published:2020-10-29

Abstract:

Three Permian-Triassic claystone are outcropped at Guanba (Qianxi County) in Guizhou Province, geologically in the southwestern South China block. One sample for zircon U-Pb dating and 7 samples for geochemical analysis were collected from the base of the claystone. LA-ICP-MS zircon U-Pb analysis shows that the zircons have 60.26×10 -6-297.90×10 -6 U and 46.14×10 -6-244.26×10 -6 Th, with Th/U value of 0.76-1.55, resembling typical igneous zircons. Zircon U-Pb dating yielded a 206Pb/ 238U weighted mean age of (252.6±1.4) Ma, and the concordant age of (252.7±0.6) Ma. Geochemical analysis shows that the tuff contains calc-alkaline volcanic materials with high Si-Al-K-Mg contents and low Fe-Ti contents. Additionally, the claystone has relatively high total REE contents, with elevated LREE enrichments and REE fractionation. Negative Eu anomaly is obvious (δEu=0.19-0.45). Geochemical characteristics indicate that the Permian-Triassic boundary at Guanba is comparable to the marine-facies Permian-Triassic boundary at Changhsing (GSSP, southeastern South China block).

Key words: Permian-Triassic boundary, claystone, LA-ICP-MS zircon U-Pb dating, Guanba area, Guizhou Province

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