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Browsing by Author Chichorro, M.

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Issue DateTitleAuthor(s)
May-2012Detrital zircon from a late Paleozoic accretionary complex of SW Iberia (Variscan Belt): History of crustal growth and recycling at the Rheic convergent marginPereira, M.F.; Drost, K.; Chichorro, M.; Silva, J.B.; Sola, R.
2012Early carboniferous wrenching, exhumation of high-grade metamorphic rocks and basin instability in SW Iberia: Constraints derived from structural geology and U–Pb and 40Ar–39Ar geochronologyPereira, M. Francisco; Chichorro, M.; Silva, J. Brandão; Ordonez-Casado, B.; Lee, James K.W.; Williams, Ian S.
2012Geologia de Portugal - Geologia Pré-Mesozóica de Portugal II.2.3. Maciço de ÉvoraPereira, M.F.; Chichorro, M.; Moita, P.; Brandão, J.B; Santos, J.F.
2012North-Gondwana assembly, break-up and paleogeography: U–Pb isotope evidence from detrital and igneous zircons of Ediacaran and Cambrian rocks of SW IberiaPereira, M.F.; Solá, A.R.; Chichorro, M.; Lopes, L.; Gerdes, A.; Silva, J.B.
2013Permo-Carboniferous magmatism in the core of Pangaea (Southern Pyreness): a possible linkange between the Variscan and Cimmerian cycles?Pereira, M Francisco; Castro, A.; Chichorro, M.; Fernandez, C.; Diaz-Alvarado, J.; Marti, J.; Rodriguez, C.
24-Apr-2014Provenance Analysis of the Late Ediacaran Basins from Southwestern Iberia (Série Negra Succession and Beiras Group): Evidence for a Common Neoproterozoic EvolutionLopes, Luís; Pereira, M. F.; Chichorro, M.; Solá, A. R.; Hofmann, M.; Linnemann, U.; Silva, J. B.; Gerdes, A.; Medina, J.
24-Apr-2014Provenance Analysis of the Late Ediacaran Basins from Southwestern Iberia (Série Negra Suecession and Beiras Group): Evidence for a Common Neoproterozoic EvolutionLopes, Luís; Pereira, M. F.; Solá, A. R.; Chichorro, M.; Medina, J.; Silva, J. B.; Gerdes, A.; Hofmann, M.; Linnemann, U.
24-Apr-2014Provenance of Cambrian–Ordovician Siliciclastic Rocks of Southwestern Iberia: Insights into the Evolution of the North Gondwana MarginLopes, Luís; Pereira, M. F.; Solá, A. R.; Chichorro, M.; Medina, J.; Silva, J.B.; Gerdes, A.; Linnemann, U.; Hofmann, M.
21-Jan-2016Provenance of upper Triassic sandstone, southwest Iberia (Alentejo and Algarve basins): tracing variability in the sourcesPereira, M. F.; Ribeiro, C.; Gama, C.; Drost, K.; Chichorro, M.; Vilallonga, F.; Hofmann, M.; Linnemann, U.
14-Jul-2014Sedimentary record of the amalgamation and break-up of Pangea: U-Pb detrital zircon geochronology and provenance of Carboniferous-Triassic siliciclastic rocks, SW IberiaPereira, M. F.; Chichorro, M.; Gutiérrez-Alonso, G.; Gama, C.; Drost, K.; Ribeiro, C.; Albardeiro, L.; Hofmann, M.; Linnemann, U.
2019The Cambrian-Early Ordovician Rift Stage in the Gondwanan Units of the Iberian Massif. In: Quesada C., Oliveira J. (eds) The Geology of Iberia: A Geodynamic Approach, Vol.2, Cap.2Sanchez-Garcia, T.; Chichorro, M.; Solá, R.; Alvaro, J.-J.; Diez-Montes, A.; Bellido, F.; Ribeiro, M.L.; Quesada, C.; Lopes, J.C.; Silva, I.F.D.; Clavijo, E.G.; Barreiro, J.G.; López-Carmona, A.
2012The missing Rheic Ocean magmatic arcs: Provenance analysis of Late PaleozoicPereira, M.F.; Chichorro, M.; Johnston, S.T.; Gutierrez-Alonso, G.; Silva, J.B.; Linnemann, U.; Hofmann, M.; Drost, K.
2012The provenance of Late Ediacaran and Early Ordovician siliciclastic rocks in the Southwest Central Iberian Zone: Constraints from detrital zircon data on northern Gondwana margin evolution during the late NeoproterozoicPereira, M.F.; Linnemann, U.; Hofmann, M.; Chichorro, M.; Solá, A.R; Medina, J.; Silva, J.B.
2010The role of the Ibero-Armorican arc in the tectonic inversion of the Sout-Portuguese Zone (SW Iberian Massif, Variscan Orogeny)Pereira, M. Francisco; Silva, J.B.; Chichorro, M.
2019Variscan MetamorphismRibeiro, M. L.; Reche, J.; López-Carmona, A.; Aguilar, C.; Bento dos Santos, T.; Chichorro, M.; Dias da Silva, I.; Díez-Montes, A.; González-Clavijo, E.; Gutiérrez-Alonso, G.; Leal, N.; Liesa, M.; Martínez, F. J.; Mateus, A.; Mendes, M. H.; Moita, P.; Pedro, Jorge; Quesada, C.; Santos, J. F.; Solá, R.; Valverde-Vaquero, P.
Showing results 1 to 15 of 15

 

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