Registros del 1 al 9 de 9 encontrados |
1.- A high resolution history of the El Nino-Southern Oscillation and of the solar activity during the late glacial-early Holocene in the subtropical Andean region Copernicus GmbH on behalf of the European Geosciences Union (EGU); Katlenburg-Lindau; DEU; Germany, 2009 European Geosciences Union general assembly 2009 Ver registro
2.- DEGREE OF POLARIZATION FILTER FOR FREQUENCY-DEPENDENT SIGNAL ENHANCEMENT THROUGH NOISE SUPPRESSION SEISMOLOGICAL SOCIETY OF AMERICA; BERKELEY, CA; USA; UNITED STATES, 2004 Ver registro
3.- Frequency-dependent phase coherence for noise suppression in seismic array data American Geophysical Union; Washington, DC; USA; United States, 2007 Ver registro
4.- INTRAPLATE SEISMICITY IN SE BRAZIL; A TREND OF HIGHER ACTIVITY IN AREAS OF THINNER LITHOSPHERE AMERICAN GEOPHYSICAL UNION; WASHINGTON, DC; USA; UNITED STATES, 2002 AGU 2002 FALL MEETING Ver registro
5.- New frequency-dependent coherence measure for noise suppression in seismic array data American Geophysical Union; Washington, DC; USA; United States, 2005 AGU 2005 fall meeting Ver registro
6.- Regional seismic tomography in Brazil and uncertainty evaluation through jackknife re-sampling method American Geophysical Union; Washington, DC; USA; United States, 2007 AGU 2007 joint assembly Ver registro
7.- SEISMIC VELOCITY ANOMALIES BENEATH SE BRAZIL FROM P AND S WAVE TRAVEL TIME INVERSIONS AMERICAN GEOPHYSICAL UNION; WASHINGTON, DC; USA; UNITED STATES, 2003 Ver registro
8.- Upper mantle anisotropy in South America with SKS splitting; predominance of asthenospheric flow from absolute plate motion and test of the frequency-dependent polarization filter in the SKS analysis American Geophysical Union; Washington, DC; USA; United States, 2007 AGU 2007 fall meeting Ver registro
9.- Using instantaneous phase coherence for signal extraction from ambient noise data at a local to a global scale Wiley-Blackwell on behalf of The Royal Astronomical Society, the Deutsche Geophysikalische Gesellsch, 2011 Ver registro
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