RT Journal Article
T1 Magmatismo postorogénico y anorogénico en el Sistema Central Español
T1 Postorogenic and anorogenic magmatism in the Spanish Central System
A1 Villaseca, Carlos
A1 Huertas, María José
A1 Nuez, J. de la
AB This work is a summary of the last magmatism in the Spanish Central System, which range in age from Permian to Jurassic times. During Permian the magmas change from peraluminous and calcalkaline to shoshonitic affinities, essentially as small plutons and later dike intrusions. This postorogenic magmatism could be related to latehercynian shear faults. At Iower Mesozoic age there are some dike intrusions ofalka/ine to tholeitic magmas in an anorogenic environnement related to Pangea transform zones of pre-At/antic opening
PB Sociedad Geológica de España
YR 1991
FD 1991
LK http://hdl.handle.net/10272/18001
UL http://hdl.handle.net/10272/18001
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 30 may 2026