内蒙古莫尔道嘎佳疙瘩组变质岩地球化学特征及构造意义

王照元; 郑常青; 徐久磊; 韩晓萌; 张慧明

doi:10.3799/dqkx.2018.011

Volume 43 Issue 1

Jan. 2018

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Article Navigation > Earth Science > 2018 > 43(1): 176-198

Wang Zhaoyuan, Zheng Changqing, Xu Jiulei, Han Xiaomeng, Zhang Huiming, 2018. Geochemistry and Its Tectonic Implictions of Metamorphic Rocks of Jiageda Formation in Moerdaoga Area, Inner Mongolia. Earth Science, 43(1): 176-198. doi: 10.3799/dqkx.2018.011

Citation:

Wang Zhaoyuan, Zheng Changqing, Xu Jiulei, Han Xiaomeng, Zhang Huiming, 2018. Geochemistry and Its Tectonic Implictions of Metamorphic Rocks of Jiageda Formation in Moerdaoga Area, Inner Mongolia. Earth Science, 43(1): 176-198. doi: 10.3799/dqkx.2018.011

Citation:

Wang Zhaoyuan, Zheng Changqing, Xu Jiulei, Han Xiaomeng, Zhang Huiming, 2018. Geochemistry and Its Tectonic Implictions of Metamorphic Rocks of Jiageda Formation in Moerdaoga Area, Inner Mongolia. Earth Science, 43(1): 176-198. doi: 10.3799/dqkx.2018.011

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Geochemistry and Its Tectonic Implictions of Metamorphic Rocks of Jiageda Formation in Moerdaoga Area, Inner Mongolia

doi: 10.3799/dqkx.2018.011

Key Laboratory of Mineral Resources Evaluation in Northeast Asia, Ministry of Land and Resources; College of Earth Sciences, Jilin University, Changchun 130061, China

Received Date: 2017-08-10
Publish Date: 2018-01-15

Abstract

Abstract

The Moerdaoga area is situated in the central-northern Erguna block, where a set of low-medium grade metamorphic rocks of Jiageda Formation develops, such as phyllites, mica schists and metamorphic sandstones. However, the origin, source and sedimentary environment of the protolith are not clear yet. The results of the major and trace elements analysis and LA-ICP-MS zircon U-Pb dating in this study show that phyllite and mica schists are enriched in Al and K and metamorphic sandstones are enriched in Si. These three groups exhibit similarity in trace element geochemistry, with strong enrichment in light REEs and negative Eu anomalies. The primitive mantle-normalized trace element pattern shows strong depletion in Sr. Furthermore, Nb, Ta, P, Ti are relatively depleted, and most high field-strength elements are enriched. The protoliths of the studied samples are mainly sandy sedimentary rocks with a small amount of muddy sedimentary rocks. The sediments show low maturity with moderate chemical weathering. The uppercrust felsic sources with possible old sediment component make a contribution to their provenance. The tectonic discrimination diagrams show that the protoliths were deposited in an active continental margin setting and had a large number of clastic rocks deposited in continental island arc setting. Most detrital zircons are of magmatic origin. The detrital zircon ages show great variations, yet mainly concentrated in Neoproterozoic (1.0-0.8 Ga) and Paleoproterozoic (2.0-1.8 Ga), which suggests that they provided the main sedimentary materials.
- Jiageda Formation,
- geochemistry,
- detrital zircon,
- petrology,
- Moerdaoga,
- Inner Mongolia

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References(140)

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