Deciphering fluid flow at the magmatic-hydrothermal transition: case of the world-class W-Sn-(Cu) ore deposit of Panasqueira (Portugal) Deciphering the behavior of fluid flow at the magmatic-hydrothermal transition is crucial to understand physical processes leading to the formation of intrusion-related ore deposits and hence to predict the localization of mineralized bodies. However, the direction and the […]
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