Galliski et al. 2011 - Valle Fértil-1
The geological setting in which pegmatite fields of muscovite class are found are well known in terms of P-T conditions. However, the tectonic setting in which they developed are less established that the ones known for rare-element class pegmatite
belts. We described a muscovite class pegmatite field that evolved in a magmatic paleoarc during the Late Cambrian to Early Ordovician Famatinian orogeny.