华北板块北缘中段花岗闪长岩-苏长辉长岩的锆石U-Pb年代学、地球化学特征及其形成机制

王师捷; 徐仲元; 董晓杰; 王挽琼; 李鹏川

doi:10.3799/dqkx.2017.585

Volume 43 Issue 9

Sep. 2018

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Article Navigation > Earth Science > 2018 > 43(9): 3267-3284

Wang Shijie, Xu Zhongyuan, Dong Xiaojie, Wang Wanqiong, Li Pengchuan, 2018. Geochemical Characteristics and Zircon U-Pb Age of the Granodiorite-Norite Gabbro in the Northern Margin of the North China Block and Their Formation Mechanism. Earth Science, 43(9): 3267-3284. doi: 10.3799/dqkx.2017.585

Citation:

Wang Shijie, Xu Zhongyuan, Dong Xiaojie, Wang Wanqiong, Li Pengchuan, 2018. Geochemical Characteristics and Zircon U-Pb Age of the Granodiorite-Norite Gabbro in the Northern Margin of the North China Block and Their Formation Mechanism. Earth Science, 43(9): 3267-3284. doi: 10.3799/dqkx.2017.585

Citation:

Wang Shijie, Xu Zhongyuan, Dong Xiaojie, Wang Wanqiong, Li Pengchuan, 2018. Geochemical Characteristics and Zircon U-Pb Age of the Granodiorite-Norite Gabbro in the Northern Margin of the North China Block and Their Formation Mechanism. Earth Science, 43(9): 3267-3284. doi: 10.3799/dqkx.2017.585

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Geochemical Characteristics and Zircon U-Pb Age of the Granodiorite-Norite Gabbro in the Northern Margin of the North China Block and Their Formation Mechanism

doi: 10.3799/dqkx.2017.585

1.
College of Earth Sciences, Jilin University, Changchun 130061, China
2.
School of Geoscience and Technology, Southwest Petroleum University, Chengdu 610500, China

Received Date: 2018-01-09
Publish Date: 2018-09-15

Abstract

Abstract

There are many acid intrusive rocks and a few norite gabbros in Tumuertai, located in central-northern margin of the North China Block. The research on the norite gabbro is limited and the evolution between the norite gabbro and cotemporary intrusive rocks has hardly been discussed. Base on the method of chronology and geochemistry, SHRIMP zircon U-Pb data indicate that the formation age of the granodiorite is 275.3±2.6 Ma; LA-ICP-MS zircon U-Pb data indicate that the formation age of the norite gabbro is 270.1±4.2 Ma, and both were formed in the Early-Permian. Geochemical data indicate that the norite gabbro is depleted in SiO₂ (46.2%-49.8%) and high field strength elements (HFSEs, e.g., Nb, Ti and Zr), and is enriched in Mg^# (59.16-67.58) and large ion lithophile elements (LILEs, e.g., Cs, Ba and Sr), and displays low REE abundances and flat REE pattern with obviously positive Eu anomalies (δEu=1.02-2.41), which is similar to mantle derived intrusive rocks. These granodiorite samples have SiO₂=65.6%-67.0%, K₂O=3.71%-4.15%, A/CNK=0.94-0.98, belong to high-K calc-alkaline I-type granitoids. They also show strong enrichments in light rare earth elements (LREEs) and LILEs (e.g., Cs, Rb and K), and depletions in HFSEs (e.g., Nb, Ta and Th) and heavy rare earth (HREEs), with weakly negative Eu anomalies (δEu=0.61-0.69). Combining with its common mafic inclusions, we consider that its primary magma could be possibly contributed by magma mixing in a continental arc setting. The spatio-temporal relationship of the granodiorite-norite gabbro and their geochemical characteristics suggest that mafic magmas derived from the depleted mantle wedge which was metasomatized by the subducted slab-derived magma. The mafic magmas not only heated to melt the crust, but also mixed with the crust-derived melts to form the diverse granitoids. In summary, we conclude that the granodiorite-norite gabbro formed in a subduction tectonic setting and the Paleo-Asian Ocean was not closed in Early Permian.
- northern margin of the North China Block,
- Early Permian intrusive rock,
- chronology,
- geochemistry,
- Paleo-Asian Ocean

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Geochemical Characteristics and Zircon U-Pb Age of the Granodiorite-Norite Gabbro in the Northern Margin of the North China Block and Their Formation Mechanism

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