| Registros del 1 al 9 de 9 encontrados |
 1.- Argon-argon ages in micas from metapelite of the Ovar-Espinho area (NW Portugal); datation of metamorphism related to the Variscan D3
[International Geological Congress]; [location varies]; III; International, 2004
Italia 2004; 32nd international geological congress; abstracts
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 2.- Confined orogen; the concept; a Precambrian example and tectonic implications
[International Geological Congress]; [location varies]; III; International, 2004
Italia 2004; 32nd international geological congress; abstracts
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 3.- Contribution of SHRIMP U/Pb zircon geochronology to unravelling the evolution of Brazilian Neoproterozoic fold belts
Elsevier; Amsterdam; III; International, 2010
The impact of SHRIMP on understanding the Precambrian
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 4.- FROM RODINIA TO GONDWANA; A REVIEW OF THE AVAILABLE EVIDENCE FROM SOUTH AMERICA
INTERNATIONAL ASSOCIATION FOR GONDWANA RESEARCH; OSAKA; JPN; JAPAN, 2003
ASSEMBLY AND BREAK-UP OF RODINIA AND GONDWANA
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 5.- K-Ar ages and REE characteristics of diagenetic clay minerals from Permian units of Parana Basin, South America
[International Geological Congress]; [location varies]; III; International, 2004
Italia 2004; 32nd international geological congress; abstracts
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 6.- Rhyacian (2.23-2.20 Ga) juvenile accretion in the southern Sao Francisco Craton, Brazil; geochemical and isotopic evidence from the Serrinha magmatic suite, Mineiro Belt
Elsevier; Oxford; GBR; United Kingdom, 2010
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 7.- The tectonic significance of juvenile intra-oceanic magmatic arcs; the case of South America
[International Geological Congress]; [location varies]; III; International, 2004
Italia 2004; 32nd international geological congress; abstracts
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 8.- U-Pb detrital zircon provenance of metasedimentary rocks from the Ceara Central and Medio Coreau Domains, Borborema Province, NE-Brazil; evidence for a long-lived Neoproterozoic active continental margin
International Gondwana Symposium; [s.l.]; III; International, 2011
Gondwana 14; abstracts
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 9.- Was there an Ediacaran Clymene Ocean in central South America?
Yale University, Kline Geology Laboratory; New Haven, CT; USA; United States, 2013
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