大别山北缘商城岩体SHRIMP锆石U-Pb年龄、地球化学及地质意义

黄丹峰; 卢欣祥; 罗照华; 宋要武; 吕国营

doi:10.3799/dqkx.2018.558

Volume 44 Issue 11

Nov. 2019

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Article Navigation > Earth Science > 2019 > 44(11): 3829-3844

Huang Danfeng, Lu Xinxiang, Luo Zhaohua, Song Yaowu, Lü Guoying, 2019. Zircon SHRIMP U-Pb Age, Geochemical Characteristics and Geological Implications of Shangcheng Pluton in the Northern Margin of Dabie Mountain. Earth Science, 44(11): 3829-3844. doi: 10.3799/dqkx.2018.558

Citation:

Huang Danfeng, Lu Xinxiang, Luo Zhaohua, Song Yaowu, Lü Guoying, 2019. Zircon SHRIMP U-Pb Age, Geochemical Characteristics and Geological Implications of Shangcheng Pluton in the Northern Margin of Dabie Mountain. Earth Science, 44(11): 3829-3844. doi: 10.3799/dqkx.2018.558

Citation:

Huang Danfeng, Lu Xinxiang, Luo Zhaohua, Song Yaowu, Lü Guoying, 2019. Zircon SHRIMP U-Pb Age, Geochemical Characteristics and Geological Implications of Shangcheng Pluton in the Northern Margin of Dabie Mountain. Earth Science, 44(11): 3829-3844. doi: 10.3799/dqkx.2018.558

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Zircon SHRIMP U-Pb Age, Geochemical Characteristics and Geological Implications of Shangcheng Pluton in the Northern Margin of Dabie Mountain

doi: 10.3799/dqkx.2018.558

1.
Henan Institute of Geological Survey, Zhengzhou 450001, China
2.
Henan Key Laboratory for Metallogenetic Process and Resources Utilization of Metallic Minerals, Zhengzhou 450001, China
3.
Scientific Academy of Land and Resources of Henan, Zhengzhou 450053, China
4.
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China

Received Date: 2018-12-08
Publish Date: 2019-11-15

Abstract

Abstract

Unconformably overlain by the Early Cretaceous volcanic rocks, the Shangcheng pluton is located in the central segment of the northern Huaiyang tectono-magmatic belt, Dabie orogen. It is of great importance to determine the emplacement age and petrogenesis of this pluton in terms of deciphering the Mesozoic tectonic evolution of the Dabie orogeny. In this paper, it reports the SHRIMP U-Pb zircon ages and whole rock geochemical data. For the central Sigudun unit of the pluton, thirteen zircon analysis spots out of fifteen yield zircon U-Pb ages of 130.2±1.7 Ma, representing the emplacement age of the pluton. The Shangcheng pluton displays high contents of Al₂O₃ and Sr, as well as high ratios of Sr/Y, and low abundances of Y and Yb, with Nb-Ta negative anomalies and pronounced LREE/HREE, but without obvious Eu anomalies (δEu=0.90~1.05), collectively pointing to an adakite affinity. Three units of Shangcheng pluton, from old to young, display a trend of gradually decreasing crystallization pressures corresponding to shallower emplacement depths step by step, suggesting that formed in an active emplacement background. The Shangcheng pluton results from the Early Cretaceous magmatic flare-up in the Dabie orogeny, and it is originated from the partial melting of the thickened lower crust. From the emplacement of the Shangcheng pluton to the eruption of the Jingangtai volcanics, this region has experienced rapid uplift and denudation. The process is exactly the surface response recorded by those two different geochemical signatures generated through thinning of the thickened lower crust. The 130 Ma is the time of tectonic regime transition of the Dabie orogen during the Mesozoic.
- Dabieshan,
- Shangcheng pluton,
- SHRIMP U-Pb zircon age,
- Early Cretaceous,
- tectonic regime transition,
- geochronology

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References(90)

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Zircon SHRIMP U-Pb Age, Geochemical Characteristics and Geological Implications of Shangcheng Pluton in the Northern Margin of Dabie Mountain

doi: 10.3799/dqkx.2018.558

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