Zeolite facies

Zeolite facies describes the mineral assemblage resulting from the pressure and temperature conditions of low-grade metamorphism.‎ The zeolite facies is generally considered to be transitional between diagenetic processes which turn sediments into sedimentary rocks, and prehnite-pumpellyite facies, which is a hallmark of subseafloor alteration of the oceanic crust around mid-ocean ridge spreading centres.‎ The zeolite and prehnite-pumpellyite facies are considered burial metamorphism as the processes of orog

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