Articles | Volume 13, issue 8
https://doi.org/10.5194/se-13-1259-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/se-13-1259-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
12 Aug 2022
Research article |
| 12 Aug 2022
| 12 Aug 2022
Whole-rock and zircon evidence for evolution of the Late Jurassic high-Sr ∕ Y Zhoujiapuzi granite, Liaodong Peninsula, North China Craton
Renyu Zeng
CORRESPONDING AUTHOR
State Key Laboratory of Nuclear Resources and Environment, East China
University of Technology, Nanchang, 330013, Jiangxi, China
School of Earth Sciences, East China University of Technology,
Nanchang, 330013, China
Department of Earth Sciences, Durham University, Durham, DH1 3LE, UK
Mark B. Allen
Department of Earth Sciences, Durham University, Durham, DH1 3LE, UK
Xiancheng Mao
School of Geosciences and Info-Physics, Central South University,
Changsha, 410083, China
Jianqing Lai
School of Geosciences and Info-Physics, Central South University,
Changsha, 410083, China
Jie Yan
State Key Laboratory of Nuclear Resources and Environment, East China
University of Technology, Nanchang, 330013, Jiangxi, China
School of Earth Sciences, East China University of Technology,
Nanchang, 330013, China
Jianjun Wan
State Key Laboratory of Nuclear Resources and Environment, East China
University of Technology, Nanchang, 330013, Jiangxi, China
School of Earth Sciences, East China University of Technology,
Nanchang, 330013, China
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Short summary
In the Liaodong Peninsula, the widely exposed Jurassic high-Sr / Y rocks are generally considered to be derived from the thickened mafic crust. However, research on the Zhoujiapuzi granite in this study shows that there is at least one pluton with a high Sr / Y signature inherited from the source. Zircon growth in Zhoujiapuzi granite can be divided into two stages. The light-CL core was formed in a deeper, hotter magma chamber. The dark-CL rim formed from later, more evolved magma.
In the Liaodong Peninsula, the widely exposed Jurassic high-Sr / Y rocks are generally...
