小兴安岭东南部伊春-鹤岗地区花岗质岩石锆石U-Pb年龄测定及其地质意义

魏红艳; 孙德有; 叶松青; 杨言辰; 刘志宏; 柳小明; 胡兆初

doi:10.3799/dqkx.2012.S1.006

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WEI Hong-yan, SUN De-you, YE Song-qing, YANG Yan-chen, LIU Zhi-hong, LIU Xiao-ming, HU Zhao-chu, 2012. Zircon U-Pb Ages and Its Geological Significance of the Granitic Rocks in the Yichun-Hegang Region, Southeastern Xiao Hinggan Mountains. Earth Science, 37(S1): 50-59. doi: 10.3799/dqkx.2012.S1.006

Citation:

WEI Hong-yan, SUN De-you, YE Song-qing, YANG Yan-chen, LIU Zhi-hong, LIU Xiao-ming, HU Zhao-chu, 2012. Zircon U-Pb Ages and Its Geological Significance of the Granitic Rocks in the Yichun-Hegang Region, Southeastern Xiao Hinggan Mountains. Earth Science, 37(S1): 50-59. doi: 10.3799/dqkx.2012.S1.006

Citation:

WEI Hong-yan, SUN De-you, YE Song-qing, YANG Yan-chen, LIU Zhi-hong, LIU Xiao-ming, HU Zhao-chu, 2012. Zircon U-Pb Ages and Its Geological Significance of the Granitic Rocks in the Yichun-Hegang Region, Southeastern Xiao Hinggan Mountains. Earth Science, 37(S1): 50-59. doi: 10.3799/dqkx.2012.S1.006

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Zircon U-Pb Ages and Its Geological Significance of the Granitic Rocks in the Yichun-Hegang Region, Southeastern Xiao Hinggan Mountains

doi: 10.3799/dqkx.2012.S1.006

1.
College of Earth Sciences, Jilin University, Changchun 130061, China
2.
State Key Laboratory of Continental Dynamics, Northwest University, Xi'an 710069, China
3.
Geological Survey of Jiangsu Province, Nanjing 210046, China
4.
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China

Received Date: 2011-05-27
Available Online: 2021-11-15
Publish Date: 2012-05-01

Abstract

Abstract

The stages of the granitoid in the Xiao Hinggan Mountains is the key to the tectonic evolution of Northeast China. Using zircon U-Pb dating results by laser ablation inductively coupled plasma mass spectrometer (LA-ICP-MS), the granitoids from Yichun-Hegang regional in the east Xiao Hinggan Mountains can be grouped into Cambrian-Ordovician (508-447 Ma), Middle-Late Permian (266-259 Ma), Early-Middle Triassic (244-231 Ma), and Late Triassic (222-200 Ma). Considering the evolution history of Xing'an-Mongolia orogenic belt (XMOB), the granitoids can be divided into different types on the basis of their Sr and Yb contents. The Middle Permian granitoids shows the characteristics of Himalayan-type granite, and was related to collision of North China craton with the Siberian craton. The Early-Middle Triassic granitoids shows the characteristics of Adakite, which originated from the thickened crust. Late Triassic granitoids shows the characteristics of Zhemin-Nanling-type granite. The formations of Triassic granitoids are related to the continued collision and extension after closure of the Paleo-Asian Ocean, respectively.
- granite,
- zircon U-Pb dating,
- Xiao Hinggan Mountains,
- tectonic setting,
- geochemistry

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References(63)

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Zircon U-Pb Ages and Its Geological Significance of the Granitic Rocks in the Yichun-Hegang Region, Southeastern Xiao Hinggan Mountains

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