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Browsing by Author Silva, J.B.

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Showing results 6 to 13 of 13
Issue DateTitleAuthor(s)
2019Revisiting the Ediacaran-Cambrian boundary in the Ossa-Morena Zone (SW Iberia)Pereira, M. F.; Dias da Silva, I.; Gama, C.; Silva, J.B.
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.
2014The Significance of Changes of Source Areas During Carboniferous Turbiditic Deposition (Southwestern Iberia)Pereira, Manuel Francisco; Chichorro, Martim; Gutierrez-Alonso, G.; Vilallonga, Filipa; Drost, K.; Ribeiro, Carlos; Silva, J.B.; Albardeiro, Luis; Hofmann, M.; Linnemann, U.
2018Time-space distribution of silicic plutonism in a gneiss dome of the Iberian Variscan Belt: The Évora Massif (Ossa-Morena Zone, Portugal)Dias da Silva, Í.; Pereira, M.F.; Silva, J.B.; Gama, C.
Mar-2018U-Pb geochronology of the El Jadida rhyolite and relation to possible Lower Cambrian recycling (Coastal block, Moroccan Meseta).Pereira, M.F.; Jouhari, A.; El Houicha, M.; Gama, C.; Ezzouhairi, H.; El Attari, A.; Fekkak, A,; Nasser, N.; Silva, J.B.
2019Zircon U-Pb geochronology and geochemistry of Cambrian magmatism in the Coastal Block (Oued Rhebar volcanic complex, Moroccan Meseta): Implications for the geodynamic evolutionary model of North-GondwanaEl Attari, A.; Pereira, M.F.; Ezzouhari, H.; El Houicha, M.; Jouhari, A.; Berrada, I.; Fekkak, A.; Ennih, N.; Hoepffner, C.H.; Gama, C.; Silva, J.B.
Showing results 6 to 13 of 13

 

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