@article{10272/10095,
year = {1999},
url = {http://hdl.handle.net/10272/10095},
abstract = {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},
publisher = {Sociedad Geológica de España},
title = {Magmatismo alcalino tardicadomiense en la zona de Ossa Morena (Macizo Ibérico): Cartografía, petrografía y geoquímica preliminar del Macizo de Almendral},
title = {The Cadomian late-orogenic alkaline magmatism in the Ossa-Morena Zone (Iberian Massif): preliminary cartography, petrography, and geochemistry of the Almedral massif},
author = {Sánchez Carretero, R. and Carracedo Sánchez, Manuel and Eguiluz, Luis and Alonso Olazabal, Ainhoa},
}