Detrital provenance of the Upper Triassic siliciclastic rocks from southwest Iberia: a review

[1] Antunes IMHR(2009)The genesis of I- and S-type granitoid rocks of the Early Ordovician Oledo pluton, Central Iberian Zone (central Portugal) Lithos 111 168-185

[2] Neiva AMR(1996)Origin of the Permian–Triassic Iberian basin, central-eastern Spain Tectonophysics 266 443-464

[3] Silva MMVG(2008)Genesis and evolution of a syn-orogenic basin in transpression: Insights from petrography, geochemistry and Sm–Nd systematics in the Variscan Pedroches basin (Mississippian, SW Iberia) Tectonophysics 461 395-413

[4] Corfu F(2010)Structural analysis of an accretionary prism in a continental collisional setting, the Late Paleozoic Pulo do Lobo Zone, Southern Iberia Gondwana Research 17 422-439

[5] Arche A(2017)Palaeogeography and crustal evolution of the Ossa-Morena Zone, Southwest Iberia, and the North Gondwana margin during the Cambro-Ordovician: A review of isotopic evidence International Geology Review 59 94-130

[6] López-Gómez J(1944)A posição estratigráfica do « Andar dos Grés de Silves» Boletim da Sociedade Geológica de Portugal, Porto 4 115-130

[7] Armendáriz M(2008)Cambrian ensialic rift-related magmatism in the Ossa-Morena Zone (Évora–Aracena metamorphic belt, SW Iberian Massif): Sm–Nd isotopes and SHRIMP zircon U–Th–Pb geochronology Tectonophysics 461 91-113

[8] López-Guijarro R(1887)Recherches sur les terrains secondaires au Sud du Sado Communicações dos Trabalhos Geológicos de Portugal I–II 222-312

[9] Quesada C(1991)The boundary between the Ossa Morena and Southportuguese Zones (Southern Iberian Massif): A major suture in the European Hercynian Chain Geologische Rundschau 80 691-702

[10] Pin C(2014)Geochemistry of the Peramora Melange and Pulo do Lobo schist: geochemical investigation and tectonic interpretation of mafic melange in the Pangean suture zone, southern Iberia International Journal of Earth Sciences 103 1415-1431

[1] Antunes IMHR(2009)The genesis of I- and S-type granitoid rocks of the Early Ordovician Oledo pluton, Central Iberian Zone (central Portugal) Lithos 111 168-185

[2] Neiva AMR(1996)Origin of the Permian–Triassic Iberian basin, central-eastern Spain Tectonophysics 266 443-464

[3] Silva MMVG(2008)Genesis and evolution of a syn-orogenic basin in transpression: Insights from petrography, geochemistry and Sm–Nd systematics in the Variscan Pedroches basin (Mississippian, SW Iberia) Tectonophysics 461 395-413

[4] Corfu F(2010)Structural analysis of an accretionary prism in a continental collisional setting, the Late Paleozoic Pulo do Lobo Zone, Southern Iberia Gondwana Research 17 422-439

[5] Arche A(2017)Palaeogeography and crustal evolution of the Ossa-Morena Zone, Southwest Iberia, and the North Gondwana margin during the Cambro-Ordovician: A review of isotopic evidence International Geology Review 59 94-130

[6] López-Gómez J(1944)A posição estratigráfica do « Andar dos Grés de Silves» Boletim da Sociedade Geológica de Portugal, Porto 4 115-130

[7] Armendáriz M(2008)Cambrian ensialic rift-related magmatism in the Ossa-Morena Zone (Évora–Aracena metamorphic belt, SW Iberian Massif): Sm–Nd isotopes and SHRIMP zircon U–Th–Pb geochronology Tectonophysics 461 91-113

[8] López-Guijarro R(1887)Recherches sur les terrains secondaires au Sud du Sado Communicações dos Trabalhos Geológicos de Portugal I–II 222-312

[9] Quesada C(1991)The boundary between the Ossa Morena and Southportuguese Zones (Southern Iberian Massif): A major suture in the European Hercynian Chain Geologische Rundschau 80 691-702

[10] Pin C(2014)Geochemistry of the Peramora Melange and Pulo do Lobo schist: geochemical investigation and tectonic interpretation of mafic melange in the Pangean suture zone, southern Iberia International Journal of Earth Sciences 103 1415-1431