新太古代晚期登封地区TTG片麻岩成因及大地构造意义

康诗胜; 刘恒; 胡天杨; 孙琳; 张云飞; 刘磊

doi:10.3799/dqkx.2023.077

Volume 48 Issue 9

Sep. 2023

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Article Navigation > Earth Science > 2023 > 48(9): 3342-3359

Kang Shisheng, Liu Heng, Hu Tianyang, Sun Lin, Zhang Yunfei, Liu Lei, 2023. Petrogenesis and Geotectonica Significance of TTG Gneiss in Late Neoarchean Dengfeng Complex. Earth Science, 48(9): 3342-3359. doi: 10.3799/dqkx.2023.077

Citation:

Kang Shisheng, Liu Heng, Hu Tianyang, Sun Lin, Zhang Yunfei, Liu Lei, 2023. Petrogenesis and Geotectonica Significance of TTG Gneiss in Late Neoarchean Dengfeng Complex. Earth Science, 48(9): 3342-3359. doi: 10.3799/dqkx.2023.077

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Petrogenesis and Geotectonica Significance of TTG Gneiss in Late Neoarchean Dengfeng Complex

doi: 10.3799/dqkx.2023.077

Kang Shisheng^{1, 2
,
,},
Liu Heng^{1, 2},
Hu Tianyang^{1, 2},
Sun Lin³,
Zhang Yunfei^{1, 2},
Liu Lei^{1, 2
,
,}

1.
Key Laboratory of Metallogenic Prediction of Nonferrous Metal and Geological Environment Monitoring, Ministry of Education, Central South University, Changsha 410083, China
2.
School of Geoscience and Info-Physics, Central South University, Changsha 410083, China
3.
School of Earth Sciences and Spatial lnformation Engineering, Hunan University of Science and Technology, Xiangtan 411201, China

Received Date: 2023-02-05
Available Online: 2023-10-07
Publish Date: 2023-09-25

Abstract

Abstract

Tonalite-trondhjemite-granodiorite (TTG) is the most important component of the early continental crust of the Earth, which is closely related to the early tectonic environment and crustal differentiation process. By means of petrography, rare earth element differentiation, U-Pb age and Hf model age of zircon and trace element simulation based on the partial melting degree, this paper defines the protolith of TTG gneiss in Dengfeng area and its residual phase during partial melting. Meanwhile, zircon U-Pb dating shows that Dengfeng complex recorded two TTG magmatism (2.57-2.55 Ga and 2.55-2.51 Ga). TTG in Dengfeng complex has high ε_Hf(t) and ε_Nd(t) values (1.7-9.7 and 0.23-3.87), which are close to the depleted mantle values of the same period. In addition, TTG gneiss has high SiO₂, Na₂O, La/Yb and Sr/Y ratios and low Mg^#, Cr, Ni, Yb, and Y contents. These data indicate that the rocks in the Dengfeng area represent the main components of mature crust. It is suggested by various data, including rock types, structural patterns, and geochemistry, that the greenstone belt combination (metamorphic volcanic sedimentary rocks) within the Dengfeng complex is forearc and accretionary terranes. The TTG-dominated Dengfeng complexes in the eastern and western parts may represent the island arc's core, and they collectively constitute the signature product of plate convergence. Further simulations of trace elements indicate that TTG gneisses in the Dengfeng area were partially melted from hydrated basaltic (amphibolite) rocks of the subducted oceanic crust, leaving behind garnet-bearing amphibolite residues. As such, we can infer that there was significant growth of young crust during this period, and the late Neoarchean TTG gneiss (2.57- 2.50 Ga) found along the southern margin of the North China Craton provides evidence to the formation of a new continental crust.
- North China Craton,
- TTG,
- trace element simulation,
- Hf isotope,
- continental crust evolution,
- petrology,
- geochemistry

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References(86)

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Petrogenesis and Geotectonica Significance of TTG Gneiss in Late Neoarchean Dengfeng Complex

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