扬子克拉通崆岭杂岩新太古代花岗片麻岩成因及其构造意义

邱啸飞; 杨红梅; 赵小明; 卢山松; 江拓; 段瑞春; 刘重芃; 彭练红; 魏运许

doi:10.3799/dqkx.2018.198

Volume 44 Issue 2

Feb. 2019

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Article Navigation > Earth Science > 2019 > 44(2): 415-426

Qiu Xiaofei, Yang Hongmei, Zhao Xiaoming, Lu Shansong, Jiang Tuo, Duan Ruichun, Liu Chongpeng, Peng Lianhong, Wei Yunxu, 2019. Neoarchean Granitic Gneisses in the Kongling Complex, Yangtze Craton: Petrogenesis and Tectonic Implications. Earth Science, 44(2): 415-426. doi: 10.3799/dqkx.2018.198

Citation:

Qiu Xiaofei, Yang Hongmei, Zhao Xiaoming, Lu Shansong, Jiang Tuo, Duan Ruichun, Liu Chongpeng, Peng Lianhong, Wei Yunxu, 2019. Neoarchean Granitic Gneisses in the Kongling Complex, Yangtze Craton: Petrogenesis and Tectonic Implications. Earth Science, 44(2): 415-426. doi: 10.3799/dqkx.2018.198

Citation:

Qiu Xiaofei, Yang Hongmei, Zhao Xiaoming, Lu Shansong, Jiang Tuo, Duan Ruichun, Liu Chongpeng, Peng Lianhong, Wei Yunxu, 2019. Neoarchean Granitic Gneisses in the Kongling Complex, Yangtze Craton: Petrogenesis and Tectonic Implications. Earth Science, 44(2): 415-426. doi: 10.3799/dqkx.2018.198

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Neoarchean Granitic Gneisses in the Kongling Complex, Yangtze Craton: Petrogenesis and Tectonic Implications

doi: 10.3799/dqkx.2018.198

1.
Isotope Geochemistry Laboratory, Wuhan Center of China Geological Survey, Wuhan 430205, China
2.
Research Center for Petrogenesis and Mineralization of Granitoid Rocks, China Geological Survey, Wuhan 430205, China

Received Date: 2018-12-23
Publish Date: 2019-02-15

Abstract

Abstract

This study carries out systematical geochronological and whole-rock geochemical investigations for the Neoarchean granitic gneisses of the Kongling complex, and discusses the petrogenesis and~3.0-2.6 Ga tectonic evolution of the nucleus of the Yangtze craton. The zircon LA-ICP-MS U-Pb dating reveals that the gneisses were crystallized at 2 673±39 Ma, and experienced high-pressure granulite-facies metamorphism at 2 042±27 Ma. The geochemical study illustrates an enrichment of Si and depletions of Mg, Cr and Ni, as well as negative anomalies of high field strength elements, Eu and Sr. The ε_Nd(t) values of the gneisses vary between -1.9 to -0.1 and the corresponding two-stage Nd isotopic model ages range from 3.15-3.01 Ga, combined with their relatively high calculated zircon saturation temperature (789-825℃), indicating that the Kongling Neoarchean gneisses might have formed by partial melting of juvenile felsic crustal materials under a high-temperature condition in the post-collisional extensional tectonic setting. Combined with the documented work, it is suggested that the nucleus of the Yangtze craton, represented by the Kongling complex, may fully record an~2.9-2.6 Ga orogenic-related event including earlier stage of oceanic slab subduction, middle stage of arc (or continent)-continent collision, and later stage of post-collisional extension.
- Neoarchean,
- granitic gneisses,
- Kongling complex,
- rock,
- tectonic implications

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Neoarchean Granitic Gneisses in the Kongling Complex, Yangtze Craton: Petrogenesis and Tectonic Implications

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