RT Journal Article
T1 Tipología del plutón de Campanario-La Haba: implicaciones petrogenéticas
T1 Campanario-La Haba pluton tipology: petrogenetic implications
A1 Alonso Olazabal, Ainhoa
A1 Aranguren, A.
A1 Carracedo Sánchez, Manuel
A1 Larrea Bilbao, F. J.
AB The Campanario-La Haba pluton is located in the suothern part of the Central-Iberian Zone. It is a coarse-grained 5 type granitoid with cordierite. Typologicaly, this pluton is a peraluminous granitoid , CCA type. Mineralogy and petrologycally, the Campanario-La Haba pluton is closer to the Central Extremadura Bath olith ( Cabeza de Araya type) than to the granitic unit of the Los Pedrodres Batholith (Sta. Eufemia, El Guijo, Cerro Mogabar, Cardeña)
PB Sociedad Geológica de España
YR 1996
FD 1996
LK http://hdl.handle.net/10272/12408
UL http://hdl.handle.net/10272/12408
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 31 may 2026