Prolonged Mantle Modification beneath the North China Craton: Evidence from Contrasting Mafic Dykes in Jiaodong Peninsula

Leilei Dong; Zhiming Yang; Mingchun Song

doi:10.1007/s12583-022-1737-7

Volume 34 Issue 4

Aug 2023

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Journal of Earth Science > 2023 > 34(4): 1150-1164.

Leilei Dong, Zhiming Yang, Mingchun Song. Prolonged Mantle Modification beneath the North China Craton: Evidence from Contrasting Mafic Dykes in Jiaodong Peninsula. Journal of Earth Science, 2023, 34(4): 1150-1164. doi: 10.1007/s12583-022-1737-7

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Leilei Dong, Zhiming Yang, Mingchun Song. Prolonged Mantle Modification beneath the North China Craton: Evidence from Contrasting Mafic Dykes in Jiaodong Peninsula. Journal of Earth Science, 2023, 34(4): 1150-1164. doi: 10.1007/s12583-022-1737-7

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Prolonged Mantle Modification beneath the North China Craton: Evidence from Contrasting Mafic Dykes in Jiaodong Peninsula

doi: 10.1007/s12583-022-1737-7

Leilei Dong^{1
,
,
,},
Zhiming Yang^{1, 2},
Mingchun Song^{3, 4}

1.
School of Civil and Resource Engineering, University of Science and Technology Beijing, Beijing 100083, China
2.
Key Laboratory of Deep-Earth Dynamics, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China
3.
College of Earth Sciences, Hebei GEO University, Shijiazhuang 050031, China
4.
Shandong Provincial No. 6 Exploration Institute of Geology and Mineral Resources, Weihai 264209, China

More Information

Corresponding author: Leilei Dong, leileidong@ustb.edu.cn
Received Date: 30 Jun 2022
Accepted Date: 05 Sep 2022

Available Online: 01 Aug 2023

Issue Publish Date: 30 Aug 2023

Abstract

Abstract

The nature of lithosphere mantle beneath North China Craton (NCC) has been changed during the Mesozoic. We investigated the mafic dykes in Jiaodong to put constraint on the origin of them and reveal the mantle evolution of the NCC. Zircons from Kunyushan and Nansu mafic dykes give concordia U-Pb ages of 114.9 and 52.8 Ma, respectively. The Kunyushan mafic dyke has high MgO (~8.0 wt.%) and Cr (> 380 ppm) but lower FeO (< 10 wt.%) contents. Large ion lithophile elements (LILE) are enriched compared to primitive mantle. The ε_Hf(t) values of zircons are between -15.0 and -20.1. All these geochemical data imply an old and enriched lithosphere mantle source. In contrast, the Nansu mafic dyke has lower concentrations of MgO (< 7.0 wt.%) and Cr (200 ppm–230 ppm) but higher FeO (> 11 wt.%) contents. The LILE and light rare earth elements (LREE) are not so strongly enriched relative to the mafic dyke from Kunyushan but display slight enrichment compared to the primitive mantle. Positive zircon ε_Hf(t) values are obtained (from +11.7 to +19.5, with one outlier of +3.4). It is suggested that the Nansu dyke sourced from an enriched MORB mantle and was generated by fluid flux melting.
- mafic dyke,
- Jiaodong,
- North China Craton,
- lithospheric mantle,
- zircon

Electronic Supplementary Materials: Supplementary materials (Tables S1–S3) are available in the online version of this article at https://doi.org/10.1007/s12583-022-1737-7
Conflict of Interest
The authors declare that they have no conflict of interest.

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