Instituto Geológico y Minero de España

LogoSistema de información documental - SID

 

 

 

Resultados de la consulta :
Instituto Geológico y Minero de España
 Registros del al 8 de 8 encontrados

1.-  1.88 GA OXIDIZED A-TYPE GRANITES OF THE RIO MARIA REGION, EASTERN AMAZONIAN CRATON, BRAZIL; POSITIVELY ANOROGENIC!
UNIVERSITY OF CHICAGO PRESS; CHICAGO, IL; USA; UNITED STATES, 2002
Ver registro

2.-  AN UPPER APTIAN SALINE PAN/LAKE SYSTEM FROM THE BRAZILIAN EQUATORIAL MARGIN; INTEGRATION OF FACIES AND ISOTOPES
BLACKWELL; OXFORD; GBR; UNITED KINGDOM, 2005
Ver registro

3.-  Geochemistry and zircon geochronology of the I-type high-K calc-alkaline and S-type granitoid rocks from southeastern Roraima, Brazil; Orosirian collisional magmatism evidence (1.97-1.96 Ga) in central portion of Guyana Shield
Elsevier; Amsterdam; III; International, 2007
Ver registro

4.-  GEOCHRONOLOGICAL PROVINCES OF THE AMAZONIAN CRATON
INTERNATIONAL UNION OF GEOLOGICAL SCIENCES (IUGS); OTTAWA, ON; CAN; CANADA, 1999
Ver registro

5.-  Petrogenesis of the Paleoproterozoic rapakivi A-type granites of the Archean Carajas metallogenic province, Brazil
Elsevier; Amsterdam; NLD; Netherlands, 2005
Granitic systems; a special issue in honor of Ilmari Haapala
Ver registro

6.-  SHRIMP U-PB, (SUPER 207) PB/ (SUPER 206) PB ZIRCON DATING, AND ND ISOTOPIC SIGNATURE OF THE UMBURANAS GREENSTONE BELT, NORTHERN SAO FRANCISCO CRATON, BRAZIL
ELSEVIER; OXFORD; GBR; UNITED KINGDOM, 2003
Ver registro

7.-  THE USE OF (SUPER 87) SR/ (SUPER 86) SR RATIO IN CHRONOSTRATIGRAPHIC AND PALEOENVIRONMENTAL INTERPRETATIONS; UPPER CRETACEOUS OF POTIGUAR BASIN, BRAZIL
THE PALEONTOLOGICAL SOCIETY AT THE UNIVERSITY OF TENNESSEE, DEPT. OF GEOLOGICAL SCIENCES; KNOXVILLE,, 1996
SIXTH NORTH AMERICAN PALEONTOLOGICAL CONVENTION; ABSTRACTS OF PAPERS
Ver registro

8.-  Zircon geochronology of granitoids from the western Bacaja Domain, southeastern Amazonian Craton, Brazil; Neoarchean to Orosirian evolution
Elsevier; Amsterdam; III; International, 2008
Ver registro


Nueva Búsqueda   Volver