| Registros del 1 al 10 de 18 encontrados |
1.- A FAST AND SIMPLE DIAGNOSTIC METHOD FOR IDENTIFYING TSUNAMIGENIC EARTHQUAKES
AMERICAN GEOPHYSICAL UNION; WASHINGTON, DC; USA; UNITED STATES, 1998
Ver registro
2.- A PRELIMINARY STUDY OF THE AFTERSHOCKS OF THE NORMAL-FAULTING OAXACA EARTHQUAKE OF SEP. 30, 1999 (M (SUB W) = 7.5)
SEISMOLOGICAL SOCIETY OF AMERICA; EL CERRITO, CA; USA; UNITED STATES, 2000
SEISMOLOGICAL SOCIETY OF AMERICA 2000; ABSTRACTS OF THE 95TH ANNUAL MEETING
Ver registro
3.- A SYSTEMATIC ERROR IN ESTIMATING SURFACE-WAVE GROUP-VELOCITY DISPERSION CURVES AND A PROCEDURE FOR ITS CORRECTION
SEISMOLOGICAL SOCIETY OF AMERICA; BERKELEY, CA; USA; UNITED STATES, 1999
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4.- Broadband ambient noise surface wave tomography across the United States
American Geophysical Union; Washington, DC; USA; United States, 2008
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5.- Crustal structure below the Valley of Mexico estimated from receiver functions
Seismological Society of America; Berkeley, CA; USA; United States, 2010
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6.- EVIDENCE OF LOW Q BELOW POPOCATEPETL VOLCANO, AND ITS IMPLICATION TO SEISMIC HAZARD IN MEXICO CITY
AMERICAN GEOPHYSICAL UNION; WASHINGTON, DC; USA; UNITED STATES, 2000
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7.- EVIDENCE OF THE DOMINANCE OF HIGHER-MODE SURFACE WAVES IN THE LAKE-BED ZONE OF THE VALLEY OF MEXICO
BLACKWELL SCIENCE FOR THE ROYAL ASTRONOMICAL SOCIETY, THE DEUTSCHE GEOPHYSIKALISCHE GESELLSCHAFT AND, 2001
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8.- Large slow slip events and the nonvolcanic tremor observed in the Mexican subduction zone are not of the same origin
American Geophysical Union; Washington, DC; USA; United States, 2009
AGU 2009 fall meeting
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9.- Nonvolcanic tremors and their correlation with slow slip events in Mexico
Copernicus GmbH on behalf of the European Geosciences Union (EGU); Katlenburg-Lindau; DEU; Germany, 2009
European Geosciences Union general assembly 2009
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10.- ORIGIN OF EXTENDED GROUND MOTION DURATION IN THE MEXICO CITY VALLEY FOR SUBDUCTION ZONE EARTHQUAKES
EUROPEAN GEOPHYSICAL SOCIETY; KATLENBURG-LINDAU; DEU; FEDERAL REPUBLIC OF GERMANY, 2000
EUROPEAN GEOPHYSICAL SOCIETY, 25TH GENERAL ASSEMBLY
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