RT Journal Article
T1 Caracterización geoquímica de las peridotitas del macizo de Sierra de Aguas (Málaga)
T1 Ceochemieal characterization ofthe peridotítes from thc Sierra de Aguas massif (Malaga)
A1 Esteban, José Julián
A1 Santos Zalduegui, José Francisco
A1 Cuevas, Julia
A1 Tubía, José María
AB In order to constraint geochemical differences related to the petrogenesis ofthe Ronda peridotites, major and trace elements combined with chondrite normalized REE patterns of the Sierra de Aguas Massif peridotites, near Carratraca (Málaga), have been compared with the similar published data from Sierra Bermeja Massif. The results establish a well geochemical distinction between previously petrographically identificated granular and porphyroclastic domains. The analyses also confirm that granular peridotites represent a more depleted mantle source than the porphyroclastics, apparently related with a fractional equilibrium melting process. Nevertheless, "U-shape" REE patterns and some REE ratios point to a more complex formation process
PB Sociedad Geológica de España
YR 2004
FD 2004
LK http://hdl.handle.net/10272/8917
UL http://hdl.handle.net/10272/8917
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 1 jun 2026