云开地块印支期变质-深熔作用:混合岩、片麻岩锆石U-Pb年代学和Hf同位素证据

柯贤忠; 周岱; 龙文国; 王晶; 徐德明; 田洋; 金巍

doi:10.3799/dqkx.2018.574

Volume 43 Issue 7

Jul. 2018

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Article Navigation > Earth Science > 2018 > 43(7): 2249-2275

Ke Xianzhong, Zhou Dai, Long Wenguo, Wang Jing, Xu Deming, Tian Yang, Jin Wei, 2018. Indosinian Metamorphism and Anatexis in Yunkai Massif: Evidences from Zircon Geochronology and Hf Isotopes of Migmatites and Gneisses. Earth Science, 43(7): 2249-2275. doi: 10.3799/dqkx.2018.574

Citation:

Ke Xianzhong, Zhou Dai, Long Wenguo, Wang Jing, Xu Deming, Tian Yang, Jin Wei, 2018. Indosinian Metamorphism and Anatexis in Yunkai Massif: Evidences from Zircon Geochronology and Hf Isotopes of Migmatites and Gneisses. Earth Science, 43(7): 2249-2275. doi: 10.3799/dqkx.2018.574

Citation:

Ke Xianzhong, Zhou Dai, Long Wenguo, Wang Jing, Xu Deming, Tian Yang, Jin Wei, 2018. Indosinian Metamorphism and Anatexis in Yunkai Massif: Evidences from Zircon Geochronology and Hf Isotopes of Migmatites and Gneisses. Earth Science, 43(7): 2249-2275. doi: 10.3799/dqkx.2018.574

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Indosinian Metamorphism and Anatexis in Yunkai Massif: Evidences from Zircon Geochronology and Hf Isotopes of Migmatites and Gneisses

doi: 10.3799/dqkx.2018.574

Wuhan Center of China Geological Survey, Wuhan 430205, China

Received Date: 2017-10-16
Publish Date: 2018-07-15

Abstract

Abstract

The Mesozoic tectonic evolution in Yunkai massif has always been one of hot topics in South China. Zircons from five metamorphic rocks including migmatite and gneiss and one granite from the metamorphic basement in Yunkai massif were measured by the LA-ICP-MS U-Pb dating method, yielding 7 metamorphic (anatectic) or magmatic ages (440.3±3.3 Ma, 230.2±2.9 Ma, 230.7±1.3 Ma, 459.5±2.7 Ma, 431.5±4.3 Ma, 229.2±5.4 Ma, 229.7±2.7 Ma) and 2 groups of detrital ages. Both the detrital zircons showed Archaean-Neoproterozoic age range with~1.0 Ga age peaks, which were similar with those of the Tiantangshan Group and the Yunkai Group. Together with the regional data, it was concluded that the Tiantangshan Group and the Yunkai Group, which were analogous in provenance and formed in Early Palaeozoic-Neoproterozoic, were broadly overprinted by the Indosinian metamorphism (anatexis)-deformation-fluid activities after the Caledonian tectonic-thermal events, resulting in differences in metamorphic grade and appearance. In situ zircon Lu-Hf isotopic analysis from four samples show that both the isotopic compositions of Caledonian metamorphic and anatectic zircons were similar with each other, which was ascribed to inheriting the compositions of provenance rocks, whereas the different isotopic compositions of Indosinian metamorphic and anatectic zircons could have been caused by individual mechanism of metamorphic and anatectic processes. It was inferred that the dominant Paleo-Mesoproterozoic crustal material played important role in the metamorphism and anatexis processes in Caledonian and Indosinian, and a few mantle-derived material was added in the anatectic processes in Caledonian and Indosinian with relatively remarkable contribution of mantle-derived material in Indosinian.
- zircon U-Pb geochronology,
- Hf isotopes,
- metamorphism-anatexis,
- Indosinian,
- Yunkai massif,
- geochemistry

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