Late Triassic zircon U-Pb ages and Sr-Nd-Hf isotopes of Darongshan granites in southeastern Guangxi and their geological implications

WANG Lei; LONG Wenguo; ZHOU Dai; XU Wangchun; JIN Xinbiao

2016 Vol. 35, No. 8

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WANG Lei, LONG Wenguo, ZHOU Dai, XU Wangchun, JIN Xinbiao. Late Triassic zircon U-Pb ages and Sr-Nd-Hf isotopes of Darongshan granites in southeastern Guangxi and their geological implications[J]. Geological Bulletin of China, 2016, 35(8): 1291-1303.

Citation:

WANG Lei, LONG Wenguo, ZHOU Dai, XU Wangchun, JIN Xinbiao. Late Triassic zircon U-Pb ages and Sr-Nd-Hf isotopes of Darongshan granites in southeastern Guangxi and their geological implications[J]. Geological Bulletin of China, 2016, 35(8): 1291-1303.

Late Triassic zircon U-Pb ages and Sr-Nd-Hf isotopes of Darongshan granites in southeastern Guangxi and their geological implications

1. Wuhan Institute of Geology and Mineral Resources, Wuhan 430205, Hubei, China;
2. Research Center of Granitic Petrogenesis and Mineralization, China Geological Survey, Wuhan 430205, Hubei, China;
3. Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, Hubei, China

Received Date: 10 April 2016

Revised Date: 03 May 2016

Publish Date: 15 August 2016

Abstract

Abstract

The petrogenesis and geodynamic processes of the Darongshan granite have been a subject of much controversy. In this paper, the authors report U-Pb ages and Sr-Nd-Hf isotopes for the Darongshan granite in southeastern Guangxi. LA-ICP-MS U-Pb zircon analysis yielded ²⁰⁶Pb/²³⁸U weighted mean age of 253.6±2.1Ma, 256.4±1.8Ma and 256.8±2.8Ma for three granite samples respectively, indicating that these granites are of Late Permian origin rather than the Early-Middle Triassic origin. They have relatively high ε_Nd(t) values (-9.18~-13.4) and younger Nd model ages (t_DM^c=1.55~1.84Ga), which are consistent with ε_Hf(t) values (-5.5~-6.7) and Hf model ages (T_DM2=1.64~1.71Ga), suggesting an lower crustal source mixed with the Paleo-Mesoproterozoic materials. Combined with previous studies, the authors hold that the Darongshan granitic magmatism might have been related to anatexis of the lower crust due to the subduction/collision between Indosinian block and South China plate during the Hercynian to Indosinian period.
- zircon U-Pb; Sr-Nd-Hf isotope; granite; Darongshan; southeastern Guangxi

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References

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