| Registros del 1 al 10 de 10 encontrados |
1.- Caribenorte project; future combined onshore-offshore survey in the north-eastern Caribbean Plate
Copernicus GmbH on behalf of the European Geosciences Union (EGU); Katlenburg-Lindau; DEU; Germany, 2008
European Geoscience Union general assembly 2008
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2.- CaribeNorte Project; studying the deep structure of the NE Caribbean Plate
American Geophysical Union; Washington, DC; USA; United States, 2009
AGU 2009 fall meeting
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3.- EVOLUCION GEOMORFOLOGICA DEL LLANO DE AZUA (SUR DE LA REPUBLICA DOMINICANA)
2002
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4.- NEOTECTONIC STRUCTURES AND PALEOSTRESS IN THE AZUA REGION, SOUTH-CENTRAL HISPANIOLA
1995
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5.- Present motion and deformation of the Caribbean Plate; constraints from new GPS geodetic measurements from Honduras and Nicaragua
Geological Society of America (GSA); Boulder, CO; USA; United States, 2007
Geologic and tectonic development of the Caribbean Plate boundary in northern Central America
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6.- Seismic images of the crust across the northern Beata Ridge (NE Caribbean)
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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7.- STRAIN PARTITIONING BY FORMATION OF MICROPLATES IN THE GREATER ANTILLES DUE TO COLLISION OF THE BAHAMAS BANK
GEOLOGICAL SOCIETY OF AMERICA (GSA); BOULDER, CO; USA; UNITED STATES, 1997
GEOLOGICAL SOCIETY OF AMERICA, 1997 ANNUAL MEETING
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8.- Submarine volcanic stratigraphy and the Caribbean LIP's formational environment
Geological Society of London; London; GBR; United Kingdom, 2009
The origin and evolution of the Caribbean Plate
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9.- The early-middle Eocene transition in the northwestern Caribbean; studies from Cuba, Jamaica, and the Cayman Rise
Geological Society of America (GSA); Boulder, CO; USA; United States, 2007
Geological Society of America, 2007 annual meeting
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10.- THE NEOGENE PLATE BOUNDARY READJUSTMENT IN OBLIQUE CONVERGENCE; HISPANIOLA, GREATER ANTILLES
AMERICAN GEOPHYSICAL UNION; WASHINGTON, DC; USA; UNITED STATES, 1995
AGU 1995 FALL MEETING
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