| Registros del 1 al 5 de 5 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
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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
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3.- 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
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4.- Geodynamic evolution of the SW Europe Variscides; discussion
American Geophysical Union; Washington, DC; USA; United States, 2009
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5.- 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
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