The large-scale Chuankou W deposit is located in the north part of the Nanling metallogenic
belt, South China. It comprises independent quartz vein-type scheelite and wolframite …

Wolframite-quartz vein-type tungsten deposits constitute the world's major tungsten
resources and are integral to tungsten production. A major share of this mineralization …

Most of the World's large tungsten deposits are genetically related to fluorine-rich granitic
magmas, their ores contain fluorine minerals, such as fluorite and topaz, and their host rocks …

Highly evolved granitic melts typically experience late-stage melt-melt and fluid-melt
immiscibility as well as fluid-melt and fluid-rock interaction. These processes are particularly …

Scheelite-bearing albitite is present in the form of rare, highly fractionated felsic dikes in the
world-class Zhuxi tungsten deposit. Morphologically, the Zhuxi albitite forms individual dikes …

Wolframite, a solid-solution series between hübnerite (MnWO 4) and ferberite (FeWO 4), is
the main tungsten-bearing ore mineral in vein-type tungsten deposits. Much progress has …

Understanding the speciation and thermodynamic properties of aqueous tungsten (W)
complexes under various conditions is essential for predicting W transport in hydrothermal …

The giant Dajishan W-polymetallic deposit, located in the Nanling metallogenic belt, is a
typical steeply dipping wolframite-quartz vein-type deposit. From top to bottom, the W ore …

The occurrence of either scheelite (CaWO 4) or wolframite ([Fe, Mn] WO 4) in tungsten
deposits is generally explained by the Ca content of the host rocks, but scheelite/wolframite …

The Ildeus mafic–ultramafic complex represents plutonic roots of a Triassic magmatic arc
tectonically emplaced into the thickened uppermost crust beneath the Mesozoic Stanovoy …