Magmatic evolution in the N-Gondwana margin related to the opening of the Rheic Ocean—evidence from the Upper Parautochthon of the Galicia-Trás-os-Montes Zone and from the Central Iberian Zone (NW Iberian Massif)

  1. Dias da Silva, Í.
  2. Díez Fernández, R.
  3. Díez-Montes, A.
  4. González Clavijo, E.
  5. Foster, D.A.
Aldizkaria:
International Journal of Earth Sciences

ISSN: 1437-3262,  1437-3254

Argitalpen urtea: 2016

Alea: 105

Zenbakia: 4

Orrialdeak: 1127-1151

Mota: Artikulua

DOI: 10.1007/S00531-015-1232-9 GOOGLE SCHOLAR
Datuen iturria: Scopus