大兴安岭北段免渡河地区晚石炭世二长花岗岩成因：锆石U⁃Pb年代学、Hf同位素和地球化学证据

许逢明; 孙巍; 吴大天; 王奎良; 周永恒

doi:10.3799/dqkx.2021.162

Volume 47 Issue 8

Sep. 2022

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Xu Fengming, Sun Wei, Wu Datian, Wang Kuiliang, Zhou Yongheng, 2022. The Petrogenesis of Late Carboniferous Monzogranite in Mianduhe Area, Northern Great Xing'an Range: Evidence from Zircon U⁃Pb Ages, Hf Isotopic and Geochemical Features. Earth Science, 47(8): 2839-2855. doi: 10.3799/dqkx.2021.162

Citation:

Xu Fengming, Sun Wei, Wu Datian, Wang Kuiliang, Zhou Yongheng, 2022. The Petrogenesis of Late Carboniferous Monzogranite in Mianduhe Area, Northern Great Xing'an Range: Evidence from Zircon U⁃Pb Ages, Hf Isotopic and Geochemical Features. Earth Science, 47(8): 2839-2855. doi: 10.3799/dqkx.2021.162

Citation:

Xu Fengming, Sun Wei, Wu Datian, Wang Kuiliang, Zhou Yongheng, 2022. The Petrogenesis of Late Carboniferous Monzogranite in Mianduhe Area, Northern Great Xing'an Range: Evidence from Zircon U⁃Pb Ages, Hf Isotopic and Geochemical Features. Earth Science, 47(8): 2839-2855. doi: 10.3799/dqkx.2021.162

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The Petrogenesis of Late Carboniferous Monzogranite in Mianduhe Area, Northern Great Xing'an Range: Evidence from Zircon U⁃Pb Ages, Hf Isotopic and Geochemical Features

doi: 10.3799/dqkx.2021.162

Shenyang Center of China Geological Survey, Shenyang 110034, China

Received Date: 2021-07-15
Publish Date: 2022-09-25

Abstract

Abstract

To determine the petrogenesis and tectonic setting of the Late Carboniferous monzogranite in the northern Great Xing'an Range, (Method) the paper analyzes the zircon U⁃Pb geochronology, Hf isotope and geochemistry of the monzogranite samples from Mianduhe area. The zircon U⁃Pb dating results show that the monzongranite was formed at 307⁃308 Ma, belonging to theLate Carboniferous.The characteristics of major elements reveal thatthe granite is characterized by alkali⁃rich(total alkali=7.28%⁃9.08%), high potassium (K₂O=3.45%⁃5.54%) and weak peraluminous (A/CNK=1.02⁃1.19), suggesting that it can be classified as high potassium calc⁃alkaline Ⅰ⁃type granite.The characteristics of trace elements reveal thatthe granite has medium⁃negative Eu anomaly(δEu=0.29⁃0.77), obviously enriched LILES(Rb, K, Th and U)and LREE, significantly depleted HFSEs(Ti, Ta and Nb) and P. In addition, the Hf isotope characteristics show that the ε_Hf(t) values range from +7.73 to +12.46, with the t_DM2 age of 501⁃764 Ma, indicating that their parent magma was formed by partial melting of the Neoproterozoic juvenile lower crust under the amphibolite facies, and then experienced significant fraction crystallization.Combined with previous study, it is suggested that the Mianduhe monzogranite was responded for the collage of the Erguna⁃Xing'an block and the Songnen block in an post⁃collision setting during the Late Carboniferous.
- monzogranite,
- zircon U-Pb chronology,
- Hf isotope,
- geochemistry,
- petrogenesis,
- tectonic setting

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致谢: 杨晓平教授级高工、郭磊研究员审阅了全稿并提出了许多建设性修改意见；马永非高工在成文过程中给予许多指导；编委及两位审稿人审阅了全文，提出了宝贵的修改意见，在此一并致以诚挚的感谢.

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