RT Journal Article
T1 Los diques alcalinos de pórfidos monzo-sieníticos del SistemaCentral Español: relación con los diques lamprofídicosacompañantes
A1 Orejana García, David
A1 Villaseca González, Carlos
AB The alkaline monzo-syenitic porphyries from the Spanish Central System (SCS) show a heterogeneouscomposition ranging from basic to acid terms which give rise to major and trace element compositionaltrends in accordance with fractional crystallization of amphibole, plagioclase, biotite, alkaline feldspar, Timagnetiteand apatite. The whole-rock geochemistry of the basic porphyries shows clear similarities withrespect to the SCS isotopically enriched alkaline lamprophyres, indicating that a genetic link between bothgroups of dykes might exist. This relationship would probably represent an origin of the monzo-syeniticporphyries after differentiation of parental lamprophyric magmas due to fractional crystallization
PB Sociedad Geológica de España
SN 0213-683X
YR 2006
FD 2006
LK https://hdl.handle.net/20.500.14352/49612
UL https://hdl.handle.net/20.500.14352/49612
LA spa
DS Docta Complutense
RD 20 mar 2026