U–Pb dating of zircons from tuff layer, sandstone and tillite samples in the uppermost Liantuo Formation and the lowermost Nantuo Formation in Three Gorges area, South China

Uranium-lead (U–Pb) dating was conducted on zircons in tuff layers and sandstone samples from the uppermost Liantuo Formation and in a tillite sample from the lowermost Nantuo Formation in Three Gorges area, South China, using SHRIMP and LA-ICP-MS techniques. Zircons from these samples yielded age s...

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Published inChemie der Erde Vol. 76; no. 1; pp. 103 - 109
Main Authors Pi, Dao-Hui, Jiang, Shao-Yong
Format Journal Article
LanguageEnglish
Published Elsevier GmbH 01.03.2016
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Abstract Uranium-lead (U–Pb) dating was conducted on zircons in tuff layers and sandstone samples from the uppermost Liantuo Formation and in a tillite sample from the lowermost Nantuo Formation in Three Gorges area, South China, using SHRIMP and LA-ICP-MS techniques. Zircons from these samples yielded age spectrum (within 1000Ma) of ∼890, ∼830, ∼780, ∼730, and 646Ma. Zircons from the Liantuo tuffs have a weighted mean 206Pb/238U age of 734.1±8.1Ma (2σ, n=7, MSWD=0.48), which was regarded as the best estimation of the upper boundary age of the Liantuo Formation. Combining with previous geochronologic data, the Liantuo Formation was proposed to be a pre-Chang′an glaciation unit, and it is comparable to the middle-upper Banxi/Danzhou Group in South China.
AbstractList Uranium-lead (U–Pb) dating was conducted on zircons in tuff layers and sandstone samples from the uppermost Liantuo Formation and in a tillite sample from the lowermost Nantuo Formation in Three Gorges area, South China, using SHRIMP and LA-ICP-MS techniques. Zircons from these samples yielded age spectrum (within 1000Ma) of ∼890, ∼830, ∼780, ∼730, and 646Ma. Zircons from the Liantuo tuffs have a weighted mean 206Pb/238U age of 734.1±8.1Ma (2σ, n=7, MSWD=0.48), which was regarded as the best estimation of the upper boundary age of the Liantuo Formation. Combining with previous geochronologic data, the Liantuo Formation was proposed to be a pre-Chang′an glaciation unit, and it is comparable to the middle-upper Banxi/Danzhou Group in South China.
Author Jiang, Shao-Yong
Pi, Dao-Hui
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  organization: State Key Laboratory of Geological Processes and Mineral Resources, Collaborative Innovation Center for Exploration of Strategic Mineral Resources, Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, PR China
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  givenname: Shao-Yong
  surname: Jiang
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  email: shyjiang@cug.edu.cn
  organization: State Key Laboratory of Geological Processes and Mineral Resources, Collaborative Innovation Center for Exploration of Strategic Mineral Resources, Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, PR China
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Keywords Liantuo Formation
Three Gorges
South China
U–Pb dating
Zircon
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Snippet Uranium-lead (U–Pb) dating was conducted on zircons in tuff layers and sandstone samples from the uppermost Liantuo Formation and in a tillite sample from the...
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StartPage 103
SubjectTerms Liantuo Formation
South China
Three Gorges
U–Pb dating
Zircon
Title U–Pb dating of zircons from tuff layer, sandstone and tillite samples in the uppermost Liantuo Formation and the lowermost Nantuo Formation in Three Gorges area, South China
URI https://dx.doi.org/10.1016/j.chemer.2015.12.003
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