浙赣三山地区早-中奥陶世斑脱岩SHR IMP锆石U-Pb精确定年

唐增才; 刘风龙; 董学发; 余盛强; 赵旭东; 胡开明; 陈忠大; 吴小勇

doi:10.3799/dqkx.2018.255

Volume 44 Issue 9

Sep. 2019

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Article Navigation > Earth Science > 2019 > 44(9): 2963-2977

Tang Zengcai, Liu Fenglong, Dong Xuefa, Yu Shengqiang, Zhao Xudong, Hu Kaiming, Chen Zhongda, Wu Xiaoyong, 2019. SHRIMP U-Pb Zircon Dating for the Early-Middle Ordovician K-Bentonites in Jiangshan-Changshan-Yushan, Zhejiang-Jiangxi Border Area. Earth Science, 44(9): 2963-2977. doi: 10.3799/dqkx.2018.255

Citation:

Tang Zengcai, Liu Fenglong, Dong Xuefa, Yu Shengqiang, Zhao Xudong, Hu Kaiming, Chen Zhongda, Wu Xiaoyong, 2019. SHRIMP U-Pb Zircon Dating for the Early-Middle Ordovician K-Bentonites in Jiangshan-Changshan-Yushan, Zhejiang-Jiangxi Border Area. Earth Science, 44(9): 2963-2977. doi: 10.3799/dqkx.2018.255

Citation:

Tang Zengcai, Liu Fenglong, Dong Xuefa, Yu Shengqiang, Zhao Xudong, Hu Kaiming, Chen Zhongda, Wu Xiaoyong, 2019. SHRIMP U-Pb Zircon Dating for the Early-Middle Ordovician K-Bentonites in Jiangshan-Changshan-Yushan, Zhejiang-Jiangxi Border Area. Earth Science, 44(9): 2963-2977. doi: 10.3799/dqkx.2018.255

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SHRIMP U-Pb Zircon Dating for the Early-Middle Ordovician K-Bentonites in Jiangshan-Changshan-Yushan, Zhejiang-Jiangxi Border Area

doi: 10.3799/dqkx.2018.255

1.
Zhejiang Institute of Geological Survey, Hangzhou 311203, China
2.
School of Earth Sciences, China University of Geosciences, Wuhan 430074, China

Received Date: 2017-05-27
Publish Date: 2019-09-15

Abstract

Abstract

There are no exact isotopic age data for "Golden Spike" in Jiangshan-Changshan-Yushan, Zhejiang-Jiangxi border area. The analysis of SHRIMP U-Pb zircons from the Ningkuo Formation K-bentonites in Jiangshan-Changshan-Yushan, yielded the age of middle Azygograptus suecicus Zone as 482.9±6.1 Ma, bottom Exigraptus clavus Zone as 477.6±8.3 Ma, and the middle Acrograptus ellesae Zone as 467.0±4.4 Ma, which provides the basis for exact correlation from the GSSP of Dapingian and Darriwilian strata in South China to other areas. Combined with contrast of biozones, the general strata-lost events occurred from 482.9 Ma to 477.6 Ma in West Zhejiang, which equated to the lacuna of the Oepikodus evae Zone to the Lenodus anticariabilis Zone, or Azygograptus suecicus Zone to Acrograptus ellesae Zone in Hangzhou-Jiaxing platform. We consider that it embodied the Yunan Movement in West Zhejiang, and heralded the start of the Early Paleozoic tectonic movement in South China, while responding to the Humberian Movement and Tactonic Movement in the European Caledonian Orogeny.
- chronology,
- geochemistry,
- K-bentonites,
- Ordovician,
- regional tectonic movement,
- Jiangshan-Changshan-Yushan area

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References(67)

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SHRIMP U-Pb Zircon Dating for the Early-Middle Ordovician K-Bentonites in Jiangshan-Changshan-Yushan, Zhejiang-Jiangxi Border Area

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