| Registros del 1 al 10 de 75 encontrados |
1.- A SEISMIC ATTENUATION ZONE BELOW POPOCATEPETL VOLCANO INFERRED FROM CODA WAVES OF LOCAL EARTHQUAKES
2005
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2.- A theory for microtremor H/V spectral ratio; application for a layered medium
Wiley-Blackwell on behalf of The Royal Astronomical Society, the Deutsche Geophysikalische Gesellsch, 2011
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3.- A WARNING MODEL BASED ON TEMPORAL CHANGES OF CODA Q FOR VOLCANIC ACTIVITY AT NEVADO DEL RUIZ VOLCANO, COLOMBIA
SPRINGER INTERNATIONAL [FOR THE] INTERNATIONAL ASSOCIATION OF VOLCANOLOGY AND CHEMISTRY OF THE EARTH, 2002
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4.- Along-strike variations of earthquake apparent stress at the Nicoya Peninsula, Costa Rica, subduction zone
American Geophysical Union and The Geochemical Society;; USA; United States, 2011
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5.- ANALISIS DE Q CODA EN LAS BETICAS CENTRALES CON DATOS DIGITALES
1991
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6.- Analysis of apparent stress for subduction zone earthquakes along the Nicoya Peninsula, Costa Rica
MARGINS Office;; USA; United States, 2008
The next decade of the Seismogenic Zone Experiment; abstract volume
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7.- ANALYSIS OF THE SPATIAL AND TEMPORAL DISTRIBUTION OF THE 2001 EARTHQUAKES IN EL SALVADOR
GEOLOGICAL SOCIETY OF AMERICA (GSA); BOULDER, CO; USA; UNITED STATES, 2004
NATURAL HAZARDS IN EL SALVADOR
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8.- ANELASTIC ATTENUATION IN THE NORTH OF PORTUGAL
EUROPEAN GEOPHYSICAL SOCIETY; KATHLENBURG-LINDAU; DEU; FEDERAL REPUBLIC OF GERMANY, 1998
23RD GENERAL ASSEMBLY OF THE EUROPEAN GEOPHYSICAL SOCIETY; PART 1, SOCIETY SYMPOSIA, SOLID EARTH, GEOPHYSICS AND GEODESY
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9.- APPLICATION OF CODA WAVE ANALYSIS TO MICROEARTHQUAKE ANALOGDATA;
1984
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10.- ARE LONG-PERIOD BODY WAVE CODA CAUSED BY LATERAL HETEROGENEITY?
1990
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