Age and Geochemistry of Late Jurassic Mafic Volcanic Rocks in the Northwestern Erguna Block, Northeast China
Abstract
:1. Introduction
2. Geological Setting and Sample Descriptions
3. Methods
4. Results
4.1. Zircon U-Pb Ages
4.2. Whole-Rock Major and Trace Element Composition
5. Discussion
5.1. Ages of Mafic Volcanic Rocks
5.2. Petrogenesis and the Nature of the Magma Source
5.3. Tectonic Background of Andesite Formation
6. Conclusions
- (1)
- The mafic volcanic rocks of the Badaguan area in the northern part of the Da Xing’anling Mountains region formed during the Late Jurassic (157–161 Ma).
- (2)
- These rocks likely derived from the partial melting of the lithosphere, previously metasomatized by subduction-related fluid with some contribution of subducted sediments.
- (3)
- The studied mafic volcanic rocks likely formed by lithospheric extension after the closure of the Mongol-Okhotsk Ocean.
Supplementary Materials
Author Contributions
Funding
Data Availability Statement
Acknowledgments
Conflicts of Interest
References
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Li, Y.; Nie, F.-J.; Yan, Z.-B. Age and Geochemistry of Late Jurassic Mafic Volcanic Rocks in the Northwestern Erguna Block, Northeast China. Minerals 2021, 11, 1010. https://doi.org/10.3390/min11091010
Li Y, Nie F-J, Yan Z-B. Age and Geochemistry of Late Jurassic Mafic Volcanic Rocks in the Northwestern Erguna Block, Northeast China. Minerals. 2021; 11(9):1010. https://doi.org/10.3390/min11091010
Chicago/Turabian StyleLi, Yan, Feng-Jun Nie, and Zhao-Bin Yan. 2021. "Age and Geochemistry of Late Jurassic Mafic Volcanic Rocks in the Northwestern Erguna Block, Northeast China" Minerals 11, no. 9: 1010. https://doi.org/10.3390/min11091010