João Mata

Contactos

Departamento de Geologia

Sala/Gabinete 6.2.75
Ext. Principal 26275
Telefone Direto 217500348
Email jmata@ciencias.ulisboa.pt

Carreira Docente Universitário
Categoria Professor Associado

Indicadores

ResearcherID
Orcid


Interesses Científicos

Geodinâmica Química; Petrologia Ígnea;

Basaltos de Ilhas Oceânicas


Scientific Interests

Chemical Geodynamics; Igneous Petrology; Ocean Island Basalts


Publicações selecionadas
  • Mata, J.; Alves, C.F.; Martins, L.; Miranda, R.; Madeira, J.; Pimentel, N.; Martins, S.; Azevedo, M.R.; Youbi, N.; De Min, A.; Almeida, I.M.; Bensalah, M.K. & Terrinha, P. (2015) - 40Ar/39Ar ages and petrogenesis of the West Iberian Margin onshore magmatism at the Jurassic-Cretaceous transition: geodynamic implications and assessment of open-system processes involving saline materials. Lithos 236-237, 156-172. doi:10.1016/j.lithos.2015.09.001
  • Mourão, C.; Mata, J.; Doucelance, R.; Madeira, J.; Millet, M-A. & Moreira, M. (2012) - Geochemical temporal evolution of Brava Island magmatism: constraints on the variability of Cape Verde mantle sources and on the carbonatite-silicate magma link. Chemical Geology, 334: 44-61. http://dx.doi.org/10.1016/j.chemgeo.2012.09.031
  • Madureira, P.; Mata, J.; Mattielli, N.; Queiroz, G. & Silva, P. (2011) - Mantle source heterogeneity, magma generation and magmatic evolution at Terceira Island (Azores archipelago): Constraints from elemental and isotopic (Sr, Nd, Hf, and Pb) data. Lithos, 126: 402-418. http://dx.doi.org/10.1016/j.lithos.2011.07.002
  • Martins, S.; Mata, J.; Munhá, J.; Mendes, M.H.; Maerschalk, C.; Caldeira, R. & Mattielli, N. (2010) – Chemical and mineralogical evidence of the occurrence of mantle metasomatism by carbonate-rich melts in an oceanic environment (Santiago Island, Cape Verde). Mineralogy and Petrology, 99: 43-65.
  • Mata, J.; Moreira, M.; Doucelance, R.; Ader, M. & Silva, L.C. (2010) – Noble gas and carbon isotopic signatures of Cape Verde oceanic carbonatites: Implications for carbon provenance. Earth Planet. Sci. Lett. 291: 70-83. http://dx.doi.org/10.1016/j.epsl.2009.12.052

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