| Registros del 1 al 10 de 73 encontrados |
1.- A COMPARISON OF ELECTROMAGNETIC DISTORTION AND RESOLUTION OF UPPER MANTLE CONDUCTIVITIES BENEATH CONTINENTAL EUROPE AND THE MEDITERRANEAN USING ISLANDS AS WINDOWS
ELSEVIER; AMSTERDAM; NLD; NETHERLANDS, 2002
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2.- A DIATOM-CONDUCTIVITY TRANSFER FUNCTION FOR SPANISH SALT LAKES
KLUWER ACADEMIC; DORDRECHT - BOSTON - LONDON; NLD; NETHERLANDS, 1998
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3.- A Foraminifera-based transfer function as a tool for sea-level reconstructions in the southern Bay of Biscay
Elsevier on behalf of Universite Claude Bernard, Departement des Sciences de la Terre; Lyon; FRA; Fr, 2008
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4.- A HIGH ELECTRICAL CONDUCTIVE ZONE AT LOWER CRUSTAL DEPTH BENEATH THE BETIC CHAIN (SPAIN)
ELSEVIER; AMSTERDAM; NLD; NETHERLANDS, 1999
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5.- A HIGH MOUNTAIN POLLEN-ALTITUDE CALIBRATION SET FOR PALAEOCLIMATIC USE IN THE TROPICAL ANDES
ARNOLD, A MEMBER OF THE HODDER HEADLINE GROUP; LONDON; GBR; UNITED KINGDOM, 2006
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6.- A new European testate amoebae transfer function for palaeohydrological reconstruction on ombrotrophic peatlands
John Wiley and Sons for the Quaternary Research Association; Chichester; GBR; United Kingdom, 2007
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7.- A permanent array of magnetotelluric stations located at the South American subduction zone in northern Chile
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.- A saturated excess runoff pedotransfer function for vegetated watersheds
Soil Science Society of America; Madison, WI; USA; United States, 2013
Frontiers of hydropedology in vadoze zone research
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9.- Ambient noise and site response; from estimation of site effects to determination of the subsoil structure
Springer; Dordrecht; NLD; Netherlands, 2009
Increasing seismic safety by combining engineering technologies and seismological data
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10.- Amplification phenomena observed in downhole array records generated on a subductive environment
Elsevier; Amsterdam; NLD; Netherlands, 2009
Earthquakes in subduction zones; a multidisciplinary approach
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