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Geochronological and geochemical constraints on the Wuyi tungsten metallogenic belt, South China
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DOI：10.1016/j.oregeorev.2026.107402.png)
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Abstract
En 中文
• First constrained the granite emplacement and mineralization ages for Guomuyang and Beikeng W deposits. • Granitic magmatism and W mineralization in the WYMB occurred during the Late Jurassic, close to the Nanling metallogenic belt. • Geochemical difference in mineralizing fluids led to higher WO3 reserves in Xingluokeng than in Guomuyang and Beikeng deposits.
Keywords:
Wuyi metallogenic belt
South China
Tungsten deposits
Wolframite
Magmatic-hydrothermal systems
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3.6
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6.4K
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2.2W
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