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Constraints from fluid inclusions on Be precipitation mechanism in Qingtian volcanic-intrusive Be deposit (southeastern China)
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DOI：10.1016/j.gexplo.2026.108101.png)
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Abstract
En 中文
• Homogenization temperatures and salinities of ore-forming fluids linked Be mineralization were revealed in the Qingtian Be ores • Chemical composition of individual fluid inclusions in quartz and fluorite indicated fluorine served as the crucial role during hydrothermal Be concentration • Trace element concentration ratios X/(Na+K) of fluid inclusions and δ18O values of quartz and calcite constraint on both fluid mixing and origin of Be • Reveal Be mineralization mechanism in the Qingtian volcanic-intrusive suite
Keywords:
Volcanic-intrusive type deposit
Metallogenic mechanism of Be
Origin of Be
Metallogenic potential of Be
Qingtian area
Southeastern coast of China
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