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Galliski et al. 2011 - Valle Fértil-1

Galliski et al. 2011 - Valle Fértil-1.png Galliski et al. 2011 - San Elías-1ThumbnailsGalliski et al. 2015 - La Nancy-1Galliski et al. 2011 - San Elías-1ThumbnailsGalliski et al. 2015 - La Nancy-1Galliski et al. 2011 - San Elías-1ThumbnailsGalliski et al. 2015 - La Nancy-1Galliski et al. 2011 - San Elías-1ThumbnailsGalliski et al. 2015 - La Nancy-1Galliski et al. 2011 - San Elías-1ThumbnailsGalliski et al. 2015 - La Nancy-1Galliski et al. 2011 - San Elías-1ThumbnailsGalliski et al. 2015 - La Nancy-1Galliski et al. 2011 - San Elías-1ThumbnailsGalliski et al. 2015 - La Nancy-1

Introduction:
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.