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texto impreso
The lithological and geochemical features of most of the NW Iberia ophiolites show they are not common MOR types. They instead formed in SSZ setting or during the opening of pull-apart type ephemeral basins. Perhaps the only exception is the Baz[...]texto impreso
Albert Roper, Richard ; Arenas Martín, Ricardo ; Gerdes, Axel ; Sánchez Martínez, S. ; Marko, Linda | Wiley | 2015-12The Variscan Upper Allochthon is a continental-affinity terrane that recorded a Cambrian–Ediacaran magmatic arc generation, a subsequent transition to a passive margin, and a collision-related high-P metamorphism during the Devonian–Carboniferou[...]
