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High-Cr and high-Al chromitites from the Sagua de Tánamo district, Mayarí-Cristal ophiolitic massif (eastern Cuba): Constraints on their origin from mineralogy and geochemistry of chromian spinel and platinum-group elements

EngineeringIgneous PetrogenesisGeologyChromian SpinelGeochemistryMineral GeochemistryGeochronologyTánamo DistrictEastern CubaPetrologyCratonTectonics