Registros del 1 al 7 de 7 encontrados |
1.- Crustal growth and deformational processes in the northern Gondwana margin; constraints from the Evora Massif (Ossa-Morena Zone, southwest Iberia, Portugal) Geological Society of America (GSA); Boulder, CO; USA; United States, 2007 The evolution of the Rheic Ocean; from Avalonian-Cadomian active margin to Alleghenian-Variscan collision Ver registro
2.- Detrital zircon age constraints on the sediment provenance of Variscan basins in SW Iberia; the missing Rheic Ocean magmatic arcs? International Gondwana Symposium; [s.l.]; III; International, 2011 Gondwana 14; abstracts Ver registro
3.- DEVELOPMENT OF LOCAL ORTHORHOMBIC FABRICS WITHIN A SIMPLE-SHEAR DOMINATED SINISTRAL TRANSPRESSION ZONE; THE ARRONCHES SHEARED GNEISSES (IBERIAN MASSIF, PORTUGAL) GEOLOGICAL SOCIETY OF LONDON; LONDON; GBR; UNITED KINGDOM, 2004 FLOW PROCESSES IN FAULTS AND SHEAR ZONES Ver registro
4.- Early Carboniferous wrenching, exhumation of high-grade metamorphic rocks and basin instability in SW Iberia; constraints derived from structural geology and U/Pb and (super 40) Ar- (super 39) Ar geochronology Elsevier; Amsterdam; NLD; Netherlands, 2012 Ver registro
5.- Geodynamic evolution of the SW Europe Variscides; discussion American Geophysical Union; Washington, DC; USA; United States, 2009 Ver registro
6.- Paleozoic high to low temperature deformation in the Evora Massif (Ossa Morena Zone, Portugal); pull-apart basin generation and exhumation of middle crustal metamorphic terrains [International Geological Congress]; [location varies]; III; International, 2004 Italia 2004; 32nd international geological congress; abstracts Ver registro
7.- Variscan intra-orogenic extensional tectonics in the Ossa-Morena Zone (Evora-Aracena-Lora del Rio metamorphic belt, SW Iberian Massif); SHRIMP zircon U/Th/Pb geochronology Geological Society of London; London; GBR; United Kingdom, 2009 Ancient orogens and modern analogues Ver registro
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