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Processes, such as partial melting, differentiation, assimilation, magma mixing, and liquid immiscibility, together with partition coefficients between minerals and melt, solubility, and redox conditions, are the controlling parameters for element distribution and enrichment processes. These factors can be evaluated through the geochemical variation of trace elements, such as Rare Earth Elements (REEs)...
The actual study deals with the temporal and geochemical evolution of the arc magmatism and the Cu-Mo-Au mineralization in the Neo-Tethyan belt of the Arasbaran region in northwestern Iran. The magmatic activity in this section of the Neo-Tethyan belt periodically occurred from Upper Cretaceous to Quaternary. The Cretaceous magmatic rocks are calc-alkaline to tholeiitic in nature without any mineralization...
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