RT Conference Proceedings
T1 Podiform chromitites from the Calzadilla de los Barros serpentinite, Iberian Massif, SW Spain
A1 Lunar Hernández, María Del Rosario
A1 Ortega Menor, Lorena
A1 Piña García, Rubén
A1 Gervilla, Fernando
A1 Monterrubio, Serafín
A1 Merinero, Raúl
AB Podiform chromitites occur as in situ and removed bodies in the Calzadilla de los Barros Serpentinite (Iberian Massif, SW Spain), a set of ultramafic massifs made up of partly serpentinized harzburgite with minor dunite and gabbros. They consist of massive to semi-massive chromitites, frequently with nodular texture. Chromite chemistry is characterized by high Al2O3 contents and up to 0.4 wt.% TiO2, in agreement with a MORB affinity of the parental melt. Platinum-group element abundances are similar to most Al-chromitites reported in the literature except for an unusual enrichment in Pt and Pd. High Pt and Pd values were probably caused by late metamorphic alteration.
YR 2011
FD 2011
LK https://hdl.handle.net/20.500.14352/106062
UL https://hdl.handle.net/20.500.14352/106062
LA eng
NO 11th SGA Biennial Meeting "Let´s Talk Ore Deposits".
NO Ministerio de Ciencia y Tecnología (España)
NO Ministerio de Economía y Competitividad (España)
DS Docta Complutense
RD 31 mar 2026