Registros del 1 al 8 de 8 encontrados |
1.- 300 million years of crustal recycling; the NW Argentine and N Chilean west Gondwana margin Deutsche Gesellschaft fuer Geowissenschaften; Hanover; DEU; Germany, 2010 SEPM-CES-GV (Sektion Sedimentologie) Sediment 2010; 25th sediment meeting; abstract volume Ver registro
2.- An early Ordovician tonalitic-granodioritic belt along the Schistose-Greywacke Domain of the Central Iberian Zone (Iberian Massif, Variscan Belt) Cambridge University Press; London; GBR; United Kingdom, 2012 Ver registro
3.- Distinguishing periods of crustal growth and recycling by U-Pb dating, Sr, Pb and Hf isotopes among the Eastern Cordilleran granitoids of south Peru Mineralogical Society; London; GBR; United Kingdom, 2011 Goldschmidt 2011 abstract volume Ver registro
4.- Geodynamic evolution of the early Paleozoic western Gondwana margin 14 degrees -17 degrees S reflected by the detritus of the Devonian and Ordovician basins of southern Peru and northern Bolivia Elsevier on behalf of International Association for Gondwana Research; Amsterdam and Kochi; III; Int, 2010 Ver registro
5.- Growth of the South American convergent margin (lat. 31 degrees -36 degrees S) during late Paleozoic times; a U-Pb and Hf-isotope study of detrital zircons from a fossil accretionary system Elsevier; New York, NY; III; International, 2007 Abstracts of the 17th annual V. M. Goldschmidt conference Ver registro
6.- History of crustal growth and recycling at the Pacific convergent margin of South America at latitudes 29 degrees -36 degrees S revealed by a U/Pb and Lu/Hf isotope study of detrital zircon from late Paleozoic accretionary systems Elsevier; Amsterdam; NLD; Netherlands, 2008 Ver registro
7.- Multiple accretion at the eastern margin of the Rio de la Plata Craton; the prolonged Brasiliano Orogeny in southernmost Brazil Springer International; Berlin; DEU; Germany, 2011 Multi-accretional tectonics at the Rio de la Plata Craton margins Ver registro
8.- North Gondwana assembly, break-up and paleogeography; U-Pb isotope evidence from detrital and igneous zircons of Ediacaran and Cambrian rocks of SW Iberia Elsevier on behalf of International Association for Gondwana Research; Amsterdam and Kochi; III; Int, 2012 Ver registro
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