Please use this identifier to cite or link to this item: http://hdl.handle.net/10174/27477

Title: Lithogeochemistry of metabasites from the Moura Phyllonitic Complex (Ossa Morena Zone, SW Portugal)
Authors: ROSEIRO, José
MOREIRA, Noel
FONSECA, Rita
ARAÚJO, Alexandre
MAIA, Miguel
PEDRO, Jorge
NOGUEIRA, Pedro
Keywords: Zona de Ossa-Morena
Geoquímica
Moura Phylonitoc Complex
Metabasite
Issue Date: 2019
Citation: ROSEIRO, J., MOREIRA, N., FONSECA, R., ARAÚJO, A., MAIA, M., PEDRO, J., NOGUEIRA, P. (2019), Lithogeochemistry of metabasites from the Moura Phyllonitic Complex (Ossa Morena Zone, SW Portugal). EGU General Assembly, Geophysical Research Abstracts, vol. 21, 7795.
Abstract: The Moura Phyllonitic Complex (MPC) is interpreted as a tectonic mélange that extends along the Montemor - Ficalho sector, overlaying the Relative Autochthone of the Ossa Morena Zone (Iberian Variscides, SW Portugal). Its northern boundary with the Estremoz-Barrancos sector is demarked by the Sto. Aleixo da Restauração Thrust. Generally, the MPC comprises several sericitic-chloritic and siliceous metasedimentary and metavolcanic rocks in a sheared matrix with unknown age, possible ranging from Cambrian to lower Devonian. Frequent imbrications of mafic suites with tholeiitic affinities are known within the MPC: obduction-related sequences, HP metamorphic rocks and dismembered volcanics interpreted as parautochthonous imbrications variably metamorphosed from lower-medium grade greenschist to amphibolite facies. Several of these metabasites were sampled for major and trace element ICP-OES analysis (prepared with alkaline fusion, acid digestion and cation-exchange chromatography), in order to characterize their geochemical variability and attempt to correlate with other autochthonous volcanic rocks, thus inferring their geodynamic setting.
URI: http://hdl.handle.net/10174/27477
Type: article
Appears in Collections:GEO - Artigos em Livros de Actas/Proceedings

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