RT Journal Article
T1 Magmatismo alcalino tardicadomiense en la zona de Ossa Morena (Macizo Ibérico): Cartografía, petrografía y geoquímica preliminar del Macizo de Almendral
T1 The Cadomian late-orogenic alkaline magmatism in the Ossa-Morena Zone (Iberian Massif): preliminary cartography, petrography, and geochemistry of the Almedral massif
A1 Sánchez Carretero, R.
A1 Carracedo Sánchez, Manuel
A1 Eguiluz, Luis
A1 Alonso Olazabal, Ainhoa
AB The Almendral massif is located in the north-western branch of the Olivenza-Monesterio antiform (Ossa Morena Zone, Iberian Massif, Spain). The pluton is composed by gabbros, sienites and alkaline granites which define an alkaline/transitional association. This magmatism marks the transition between the Cadomian orogenic regime and the Pre-Hercynian intracontinental rift for this sector
PB Sociedad Geológica de España
YR 1999
FD 1999
LK http://hdl.handle.net/10272/10095
UL http://hdl.handle.net/10272/10095
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 31 may 2026