@article{10272/8016,
year = {2009},
url = {http://hdl.handle.net/10272/8016},
abstract = {The metabasites cropping out in the Sierra del Algarrobo have been studied from petrological and
geochemical points of view. They consist of gabbros, dolerites and basalts, which were transformed into
eclogites or amphibolites during the Alpine metamorphism. Their primary magmas were tholeiitic basalts
originated in E-MORB to N-MORB geodynamic conditions. By comparing these metabasites with those of
the Betic and Alpine-Apennine Ophiolites and with basalts from current oceanic ridges, we classify them
as ophiolitic and tectonically deriving from the oceanic floor of the Jurassic Western Tethys},
keywords = {Betic ophiolites},
keywords = {Sierra del Algarrobo},
keywords = {Mulhacén Complex},
keywords = {Nevadofilábride Domain},
keywords = {Eastern Betic Cordillera},
title = {Caracterización geoquímica y ambiente geodinámico de génesis de las metabasitas de la Sierra del Algarrobo (Cordillera Bética oriental)},
title = {Geochemical characterization and geodynamic setting of the metabasites from Sierra del Algarrobo (eastern Betic
Cordillera)},
author = {Puga, Encarnación and Rodríguez Martínez Conde, José Ángel and Díaz de Federico, Antonio and Manteca Martínez, José Ignacio and Díaz Puga, Miguel Ángel},
}