| Registros del 1 al 10 de 462 encontrados |
1.- (super 40) Ar/ (super 39) Ar age constraints for the D2 Variscan extension in the Porto-Viseu metamorphic belt (Portugal)
Elsevier; New York, NY; III; International, 2008
Abstracts of the 18th annual V. M. Goldschmidt conference
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2.- (SUPER 40) AR/ (SUPER 39) AR DATING OF VOLCANISM AND SUBSEQUENT VERY LOW-GRADE METAMORPHISM IN A SUBSIDING BASIN; EXAMPLE OF THE CRETACEOUS LAVA SERIES FROM CENTRAL CHILE
ELSEVIER; AMSTERDAM; NLD; NETHERLANDS, 2005
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3.- 25 million years to break a continent; early to middle Miocene rifting and syn-extensional magmatism in the southern Gulf of California
Geological Society of America (GSA); Boulder, CO; USA; United States, 2012
Geological Society of America, Cordilleran Section, 108th annual meeting
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4.- 3-D CRUSTAL STRUCTURE OF THE EXTENSIONAL GRANADA BASIN IN THE CONVERGENT BOUNDARY BETWEEN THE EURASIAN AND AFRICAN PLATES
ELSEVIER; AMSTERDAM; NLD; NETHERLANDS, 2002
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5.- 3D GEOMETRY OF LATE-KINEMATIC GRANITES OF GALICIA (TOJIZA AND LUGO)
[PUBLISHER VARIES]; [LOCATION VARIES]; III; INTERNATIONAL, 2000
GALICIA 2000; VARISCAN-APPALACHIAN DYNAMICS, THE BUILDING OF THE UPPER PALEOZOIC BASEMENT
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6.- 3D shear velocity structure beneath the Gulf of California from Rayleigh wave dispersion
Elsevier; Amsterdam; NLD; Netherlands, 2009
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7.- 3D structure at the front of the Colombia-Ecuador subduction zone and relation with the 1958 earthquake rupture zone
Copernicus GmbH on behalf of the European Geosciences Union (EGU); Katlenburg-Lindau; DEU; Germany, 2010
European Geosciences Union general assembly 2010
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8.- 40Ar/39Ar ages (600-570 Ma) of the extensional structures in the southern part of the Ribeira Belt, southeastern Brazil
[International Geological Congress]; [location varies]; III; International, 2008
33rd international geological congress; abstracts
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9.- 55 MILLION YEARS OF CONTINUOUS ANATEXIS IN CENTRAL IBERIA; SINGLE-ZIRCON DATING OF THE PENA NEGRA COMPLEX
GEOLOGICAL SOCIETY OF LONDON; LONDON; GBR; UNITED KINGDOM, 2004
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10.- A "CORE-COMPLEX-LIKE STRUCTURE" FORMED BY SUPERIMPOSED EXTENSION, FOLDING AND HIGH-ANGLE NORMAL FAULTING; THE SANTI PETRI DOME (WESTERN BETICS, SPAIN)
ELSEVIER; PARIS; FRA; FRANCE, 2003
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