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Published in 2024 at "Minerals"
DOI: 10.3390/min14030261
Abstract: The Huayangchuan U-polymetallic deposit in the Qinling Orogen is a newly verified carbonatite-hosted deposit on the southern margin of the North China Craton (NCC) in Central China. Granitic magmatism is extensively developed in the Huayangchuan…
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Keywords:
deposit qinling;
qinling orogen;
magmatism;
granitic magmatism ... See more keywords