豫西小秦岭地区晚古元古代地壳深熔作用及构造意义：岩石学和锆石U-Pb年代学证据

朱越; 周汉文; 李少林; 谢瑜; 丁振举; 李建威; 姚书振

doi:10.3799/dqkx.2015.067

Volume 40 Issue 5

May 2015

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Article Navigation > Earth Science > 2015 > 40(5): 824-839

Zhu Yue, Zhou Hanwen, Li Shaolin, Xie Yu, Ding Zhenju, Li Jianwei, Yao Shuzhen, 2015. Late Paleoproterozoic Crustal Anatexis and Its Tectonic Significance: Evidence from Petrology and Zircon U-Pb Ages of Migmatite from Xiaoqinling Area, West Henan. Earth Science, 40(5): 824-839. doi: 10.3799/dqkx.2015.067

Citation:

Zhu Yue, Zhou Hanwen, Li Shaolin, Xie Yu, Ding Zhenju, Li Jianwei, Yao Shuzhen, 2015. Late Paleoproterozoic Crustal Anatexis and Its Tectonic Significance: Evidence from Petrology and Zircon U-Pb Ages of Migmatite from Xiaoqinling Area, West Henan. Earth Science, 40(5): 824-839. doi: 10.3799/dqkx.2015.067

Citation:

Zhu Yue, Zhou Hanwen, Li Shaolin, Xie Yu, Ding Zhenju, Li Jianwei, Yao Shuzhen, 2015. Late Paleoproterozoic Crustal Anatexis and Its Tectonic Significance: Evidence from Petrology and Zircon U-Pb Ages of Migmatite from Xiaoqinling Area, West Henan. Earth Science, 40(5): 824-839. doi: 10.3799/dqkx.2015.067

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Late Paleoproterozoic Crustal Anatexis and Its Tectonic Significance: Evidence from Petrology and Zircon U-Pb Ages of Migmatite from Xiaoqinling Area, West Henan

doi: 10.3799/dqkx.2015.067

1.
School of Earth Sciences, China University of Geosciences, Wuhan 430074, China
2.
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China
3.
Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China

Received Date: 2014-09-30
Publish Date: 2015-05-15

Abstract

Abstract

The Taihua Group, exposed in the southernmost terminal Trans-North China Orogen (TNCO), is important for deciphering the mysterious evolution processes of the southern margin of the North China Craton during Proterozoic, and determination of the collision time of the eastern and western blocks of the North China Craton. Petrological study on three kinds of migmatites formed by anatexis from the Taihua Group in Xiaoqinling area, West Henan, indicates that the transformation of migmatites caused by anatexis is uneven, which is obviously limited by the composition of protolith, structure of rocks and other properties. LA-ICP-MS U-Pb dating of the anatexis zircons shows that the protolith crystallized in the Paleoproterozoic and the anatexis occurred at about 1.8 Ga. The migmatites and contemporaneous mafic dike swarms and A-type granite in the study area were generated in a post-orogenic, extensional environment following continent-continent collision at 1.85 Ga between the eastern and western blocks of the North China Craton.
- Taihua Group,
- migmatite,
- anatexis,
- geochronology,
- southern margin of North China Craton,
- petrology,
- tectonics

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References(80)

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Late Paleoproterozoic Crustal Anatexis and Its Tectonic Significance: Evidence from Petrology and Zircon U-Pb Ages of Migmatite from Xiaoqinling Area, West Henan

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