| Registros del 1 al 10 de 62 encontrados |
1.- ¿QUE ES UNA ONDA? Y OTRAS CUESTIONES BASICAS
1999
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2.- A depositional model for a wave-dominated open-coast tidal flat, based on analyses of the Cambrian-Ordovician Lagarto and Palmares Formations, north-eastern Brazil
Wiley-Blackwell; Oxford; GBR; United Kingdom, 2012
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3.- Alternacia de los ciclos de erosion-acrecion de playa relacionados con el oleaje en Rosarito, Baja California, Mexico--Alternating beach erosion-accretion cycles associated with wave action off Rosarito, Baja California, Mexico
Instituto de Investigaciones Oceanologicas de la Universidad Autonoma de Baja California; Ensenada, , 2007
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4.- An algorithm for the measurement of shoreline and intertidal beach profiles using video imagery; PSDM
Elsevier; Amsterdam; NLD; Netherlands, 2012
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5.- An approximation to short-term evolution and sediment transport pathways along the littoral of Cadiz Bay (SW Spain)
Springer International; Berlin; DEU; Federal Republic of Germany, 2008
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6.- An unusual sedimentary system; the Gil Eanes Channel, Gulf of Cadiz
[International Geological Congress]; [location varies]; III; International, 2004
Italia 2004; 32nd international geological congress; abstracts
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7.- ANALISE DA POLARIZAÇAO DE ONDAS S DA SEQUENCIA SISMICA POS-SISMO DO FAIAL DE 9 DE JULHO DE 1998: RESULTADOS PRELIMINARES
UNIVERSIDAD POLITECNICA DE VALENCIA; VALENCIA;ESP, 2003
3ª ASAMBLEA HISPANO-PORTUGUESA DE GEODESIA Y GEOFISICA.. PROCEEDINGS. TOMO I
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8.- Analysis of the environmental effects of ground vibrations produced by blasting in quarries
Taylor & Francis; Abingdon; GBR; United Kingdom, 2006
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9.- Beach dynamics in the Portuguese coast; the impact of atmospheric circulation on the two major driving factors (waves and precipitation)
Copernicus GmbH on behalf of the European Geosciences Union (EGU); Katlenburg-Lindau; DEU; Federal R, 2008
European Geosciences Union general assembly 2008
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10.- C3; a finite volume-finite difference hybrid model for tsunami propagation and runup
Elsevier; Amsterdam; NLD; Netherlands, 2011
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