Yangshan A-Type Granites in the Lower Yangtze River Belt Formed by Ridge Subduction: Radiogenic Ca and Nd Isotopic Constraints

Jianghao Bai; Mingxing Ling; Xiaoyong Yang; Fang Liu; Huangling Gu; Zebin Luo; Xiaoyan Jiang; Zhaofeng Zhang

doi:10.1007/s12583-021-1588-7

Volume 33 Issue 3

Jun 2022

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Journal of Earth Science > 2022 > 33(3): 581-590.

Jianghao Bai, Mingxing Ling, Xiaoyong Yang, Fang Liu, Huangling Gu, Zebin Luo, Xiaoyan Jiang, Zhaofeng Zhang. Yangshan A-Type Granites in the Lower Yangtze River Belt Formed by Ridge Subduction: Radiogenic Ca and Nd Isotopic Constraints. Journal of Earth Science, 2022, 33(3): 581-590. doi: 10.1007/s12583-021-1588-7

Citation:

Jianghao Bai, Mingxing Ling, Xiaoyong Yang, Fang Liu, Huangling Gu, Zebin Luo, Xiaoyan Jiang, Zhaofeng Zhang. Yangshan A-Type Granites in the Lower Yangtze River Belt Formed by Ridge Subduction: Radiogenic Ca and Nd Isotopic Constraints. Journal of Earth Science, 2022, 33(3): 581-590. doi: 10.1007/s12583-021-1588-7

Citation:

Jianghao Bai, Mingxing Ling, Xiaoyong Yang, Fang Liu, Huangling Gu, Zebin Luo, Xiaoyan Jiang, Zhaofeng Zhang. Yangshan A-Type Granites in the Lower Yangtze River Belt Formed by Ridge Subduction: Radiogenic Ca and Nd Isotopic Constraints. Journal of Earth Science, 2022, 33(3): 581-590. doi: 10.1007/s12583-021-1588-7

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Yangshan A-Type Granites in the Lower Yangtze River Belt Formed by Ridge Subduction: Radiogenic Ca and Nd Isotopic Constraints

doi: 10.1007/s12583-021-1588-7

Jianghao Bai^{1, 2, 8
,},
Mingxing Ling^{3
,
,
,},
Xiaoyong Yang⁴,
Fang Liu⁵,
Huangling Gu⁶,
Zebin Luo^{1, 2, 8},
Xiaoyan Jiang⁷,
Zhaofeng Zhang^{1, 5
,
,
,}

1.
State Key Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China
2.
CAS Center for Excellence in Deep Earth Science, Guangzhou 510640, China
3.
State Key Laboratory of Nuclear Resources and Environment, East China University of Technology, Nanchang 330013, China
4.
Key Laboratory of Crust-Mantle Materials and Environments, School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, China
5.
International Research Center for Planetary Science, College of Earth Sciences, Chengdu University of Technology, Chengdu 610059, China
6.
School of City and Environment, Hunan University of Technology, Zhuzhou 412007, China
7.
State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, China
8.
University of Chinese Academy of Sciences, Beijing 100049, China

More Information

Corresponding author: Mingxing Ling, mxling@ecut.edu.cn; Zhaofeng Zhang, zzf@cdut.edu.cn
Received Date: 23 Jun 2021
Accepted Date: 13 Oct 2021

Abstract

Abstract

The Early Cretaceous aluminous A-type granites in the Lower Yangtze River belt (LYRB) can provide important insights into the Mesozoic magmatism in eastern China, but their origin remains highly controversial. In this study, radiogenic Ca-Nd isotopic analysis was performed for syenite porphyry and alkali-feldspar granite porphyry of the Yangshan pluton, a typical aluminous A-type granitic intrusion in the LYRB, to constrain its source and geodynamic setting. The results show thatε_Ca(126 Ma),ε_Nd(126 Ma) and K/Ca_source of the syenite porphyry range from -0.24 to +0.96, -7.2 to -6.0, and 0.31 to 1.26, respectively. The corresponding values for the alkali-feldspar granite porphyry range from 0.26 to 0.84, -8.0 to -6.1, and 0.79 to 1.08, respectively. Binary mixing modeling indicates that they were originated from the same sources with different proportion, namely, a mixing of 50% to 75% Neoproterozoic crust and 50% to 25% asthenospheric mantle. Together with previous works, we propose that the Early Cretaceous subduction of the ridge between the Pacific and Izanagi plates was responsible for the formation of the aluminous A-type granites in the LYRB.
- Lower Yangtze River belt (LYRB),
- aluminous A-type granite,
- Yangshan pluton,
- radiogenic Ca-Nd isotopes,
- ridge subduction,
- geochemistry

Electronic Supplementary Material: Supplementary material (Table S1) is available in the online version of this article at https://doi.org/10.1007/s12583-021-1588-7.

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