Fluid–Melt–Rock Interaction during the Transition from Magmatism to HT-UHT-Granulite- and Amphibolite-Facies Metamorphism in the Ediacaran Adrar–Suttuf Metamafic Complex, NW Margin of the West African Craton (Southern Morocco)
JosÉ Francisco Molina,
Fernando Bea,
Pilar Montero
et al.
Abstract:Underplated mafic intrusions ponded at the base of the lower continental crust in extensional settings can experience ultra-high temperature (UHT) granulite-facies metamorphism during tens of My due to slow cooling rates, being also the source of heat and carbonic fluids for regional high-temperature (HT) granulite-facies metamorphism in the continental crust. This work analyses the fluid-melt-rock interaction processes that occurred during the magmatic to HT-UHT-granulite- and amphibolite-facies metamorphic e… Show more
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