新太古代-古元古代熊耳山地区的岩浆作用与大地构造意义

刘恒; 刘磊; 张德贤; 康诗胜; 胡天杨

doi:10.3799/dqkx.2024.019

Volume 50 Issue 2

Feb. 2025

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Article Navigation > Earth Science > 2025 > 50(2): 667-686

Liu Heng, Liu Lei, Zhang Dexian, Kang Shisheng, Hu Tianyang, 2025. Magmatic Activity and Tectonic Significance in the Xiong'ershan Area during the Neoarchean to Early Paleoproterozoic. Earth Science, 50(2): 667-686. doi: 10.3799/dqkx.2024.019

Citation:

Liu Heng, Liu Lei, Zhang Dexian, Kang Shisheng, Hu Tianyang, 2025. Magmatic Activity and Tectonic Significance in the Xiong'ershan Area during the Neoarchean to Early Paleoproterozoic. Earth Science, 50(2): 667-686. doi: 10.3799/dqkx.2024.019

Citation:

Liu Heng, Liu Lei, Zhang Dexian, Kang Shisheng, Hu Tianyang, 2025. Magmatic Activity and Tectonic Significance in the Xiong'ershan Area during the Neoarchean to Early Paleoproterozoic. Earth Science, 50(2): 667-686. doi: 10.3799/dqkx.2024.019

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Magmatic Activity and Tectonic Significance in the Xiong'ershan Area during the Neoarchean to Early Paleoproterozoic

doi: 10.3799/dqkx.2024.019

Liu Heng^{1, 2
,
,},
Liu Lei^{1, 2
,
,
,},
Zhang Dexian^{1, 2},
Kang Shisheng^{1, 2},
Hu Tianyang^{1, 2}

1.
Key Laboratory of Metallogenic Prediction of Nonferrous Metals and Geological Environment Monitoring, Ministry of Education in Central South University, Changsha 410083, China
2.
School of Geosciences and Info-Physics, Central South University, Changsha 410083, China

Received Date: 2024-01-03
Publish Date: 2025-02-25

Abstract

Abstract

The ancient rocks exposed along the southern margin of the North China Craton primarily comprise a suite of rocks known as TTG (Tonalite-Trondhjemite-Granodiorite) and K-rich granites. This suite represents a critical target for the study of granite genesis and the evolution of continental crust. This paper focuses on the Xiong'ershan region and employs zircon microanalysis of Hf-O isotopes and trace elements to trace the evolution of magma. It explores the geochemical characteristics of granites at different stages, the nature of their source regions, and the mechanisms behind their formation. This study identifies two significant magmatic-tectonic events around 2.5 to 2.4 Ga and ~2.3 Ga. The research reveals that in the Xiaonangou region, trondhjemite from 2.51 to 2.43 Ga contain rich titanium oxides, with low ε_Hf(t) values ranging from -6.9 to +5.0. The zircon oxygen isotope values average 6.03‰ and 5.18‰, suggesting potential associations with partial crustal melting and the incorporation of sedimentary material. In the Huanggou and Muce regions, ~2.3 Ga potassic granites exhibit zircon oxygen isotope values averaging 3.98‰ and 3.10‰, with enriched ε_Hf(t) values ranging from -5.8 to -3.5, respectively. The significant decrease in zircon δ¹⁸O values may be linked to high-temperature hydrothermal-magmatic interactions caused by upwelling mantle material. Zircon trace element compositions of different types in granites from different eras exhibit characteristics of continental arc environments. Combined with continuously low ε_Hf(t) and reducing δ¹⁸O isotopic composition, the Xiong'ershan region likely formed in an active continental margin arc environment on the eve of the magmatic quiet period.
- zircon Hf-O isotope,
- oxygen fugacity,
- the southern margin of the NCC,
- 2.5~2.3 Ga,
- Active continental margin,
- structural geology

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References(99)

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Magmatic Activity and Tectonic Significance in the Xiong'ershan Area during the Neoarchean to Early Paleoproterozoic

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