华北克拉通南缘约2.5 Ga构造变质事件及意义

曹正琦; 翟文建; 蒋幸福; 胡正祥; 曾佐勋; 蔡逸涛; 张雄; 徐少朋; 郭君功

doi:10.3799/dqkx.2016.047

Volume 41 Issue 4

Apr. 2016

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Article Navigation > Earth Science > 2016 > 41(4): 570-585

Cao Zhengqi, Zhai Wenjian, Jiang Xingfu, Hu Zhengxiang, Zeng Zuoxun, Cai Yitao, Zhang Xiong, Xu Shaopeng, Guo Jungong, 2016. About 2.5 Ga Tectono-Metamorphic Event in Southern Margin of North China Craton and Its Significance. Earth Science, 41(4): 570-585. doi: 10.3799/dqkx.2016.047

Citation:

Cao Zhengqi, Zhai Wenjian, Jiang Xingfu, Hu Zhengxiang, Zeng Zuoxun, Cai Yitao, Zhang Xiong, Xu Shaopeng, Guo Jungong, 2016. About 2.5 Ga Tectono-Metamorphic Event in Southern Margin of North China Craton and Its Significance. Earth Science, 41(4): 570-585. doi: 10.3799/dqkx.2016.047

Citation:

Cao Zhengqi, Zhai Wenjian, Jiang Xingfu, Hu Zhengxiang, Zeng Zuoxun, Cai Yitao, Zhang Xiong, Xu Shaopeng, Guo Jungong, 2016. About 2.5 Ga Tectono-Metamorphic Event in Southern Margin of North China Craton and Its Significance. Earth Science, 41(4): 570-585. doi: 10.3799/dqkx.2016.047

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About 2.5 Ga Tectono-Metamorphic Event in Southern Margin of North China Craton and Its Significance

doi: 10.3799/dqkx.2016.047

1.
School of Earth Sciences, China University of Geosciences, Wuhan 430074, China
2.
Hubei Geological Survey, Wuhan 430034, China
3.
Henan Institute of Geological Survey, Zhengzhou 450001, China
4.
Faculty of Earth Sciences, East China University of Technology, Nanchang 330013, China
5.
Nanjing Center, China Geological Survey, Nanjing 210016, China

Received Date: 2015-07-12
Publish Date: 2016-04-15

Abstract

Abstract

Linshan Group, located in the southern margin of the central orogenic belt of the North China Craton, is a Precambrian basement. It is important to study the collision era of the central orogenic belt and the distribution of the southern margin of the North China Craton. A study was carried out on the metabasite (plagioclase-amphibole schist) of the Linshan Group for the purpose of constraining the collisional time of the central orogenic belt and its distribution through the zircon U-Pb dating and rock geochemical methods. The results obtained show that most of zircon grains from plagioclase-amphibole schist are long columnar, euhedral to subhedral, and show typical core-rim structure with irregular shape, weak zoning, taxitic zoning and sector zoning structure. Some zircons preserve the inherited cores of the early magma. Zircon rims display characteristics of dissolution texture with low Th/U ratios (most of them less than 0.09), however, zircons' cores show typical oscillatory zoning structure and relatively high Th/U ratios ranging from 0.10 to 9.24. The evidence suggests that the zircons of plagioclase-amphibole schist could be metamorphic origin. Relict cores and rims of the zircons from the plagioclase-amphibole schist yield ages of 2 528±43 Ma (MSWD=1.5, n=10) and 2 474±22 Ma (MSWD=1.3, n=21), respectively. The former data represent residual age of protolith, and the latter indicate a circa 2.5 Ga metamorphic event in the central orogenic belt of the North China Craton. Whole-rock geochemical results show that metabasite samples from the Linshan Group have relatively low contents of SiO₂ (47.70%-50.77%, average=48.90%) and K₂O (0.56%-1.78%, average=1.13%), and are depleted in high field strength elements (eg., Nb, Th, Ti and Zr) with flat REE patterns. Moreover, the geochemical samples have low content of Zr (less than 130×10^-6) and ratios of Zr/Y (less than 4), indicating that the Linshan Group could have been formed in the subducted-related island arc environment. Therefore, the above evidence show that the central orogenic belt that formed by the collision orogenesis between eastern block and western block of the North China Craton experienced late Neoarchean to early Paleoproterozoic subduction-collisional event.
- early Paleoproterozoic,
- metamorphic event,
- Linshan Group,
- North China Craton,
- central orogenic belt,
- isotope,
- tectonics

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References(98)

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About 2.5 Ga Tectono-Metamorphic Event in Southern Margin of North China Craton and Its Significance

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