Show simple item record

Ceochemieal characterization ofthe peridotítes from thc Sierra de Aguas massif (Malaga)

dc.contributor.authorEsteban, José Julián
dc.contributor.authorSantos Zalduegui, José Francisco
dc.contributor.authorCuevas, Julia
dc.contributor.authorTubía, José María
dc.description.abstractIn 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 processen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.subject.otherBetic Cordilleraen_US
dc.subject.otherRonda peridotitesen_US
dc.subject.otherMajor and trace elementsen_US
dc.titleCaracterización geoquímica de las peridotitas del macizo de Sierra de Aguas (Málaga)en_US
dc.titleCeochemieal characterization ofthe peridotítes from thc Sierra de Aguas massif (Malaga)eng

Files in this item

This item appears in the following Collection(s)

Show simple item record

Atribución-NoComercial-SinDerivadas 3.0 España
Except where otherwise noted, this item's license is described as Atribución-NoComercial-SinDerivadas 3.0 España

Copyright © 2008-2010. ARIAS MONTANO. Repositorio Institucional de la Universidad de Huelva
Contact Us | Send Feedback |