Registros del 1 al 10 de 17 encontrados |
1.- DIRECT BODY-WAVE Q ESTIMATES IN NORTHERN BAJA CALIFORNIA, MEXICO ELSEVIER; AMSTERDAM; NLD; NETHERLANDS, 1997 Ver registro
2.- Location of aftershocks of the 4 April 2010 M (sub w) 7.2 El Mayor-Cucapah earthquake of Baja California, Mexico Seismological Society of America; Berkeley, CA; USA; United States, 2011 Ver registro
3.- Location of moderate-sized earthquakes recorded by the NARS-Baja array in the Gulf of California region between 2002 and 2006 Birkhaeuser; Basel; CHE; Switzerland, 2011 Geodynamics of the Mexican Pacific margin Ver registro
4.- P- AND S-WAVE SITE RESPONSE OF THE SEISMIC NETWORK RESNOM DETERMINED FROM EARTHQUAKES OF NORTHERN BAJA CALIFORNIA, MEXICO BIRKHAEUSER VERLAG; BASEL; CHE; SWITZERLAND, 1998 Ver registro
5.- Potential signatures of damage-related radiation from aftershocks of the 4 April 2010 (M (sub w) 7.2) El Mayor-Cucapah earthquake, Baja California, Mexico Seismological Society of America; Berkeley, CA; USA; United States, 2013 Ver registro
6.- REGIONAL CRUSTAL THICKNESS VARIATIONS OF THE PENINSULAR RANGES AND GULF EXTENSIONAL PROVINCE, NORTHERN BAJA CALIFORNIA AND SOUTHERN ALTA CALIFORNIA SEISMOLOGICAL SOCIETY OF AMERICA; EL CERRITO, CA; USA; UNITED STATES, 2000 SEISMOLOGICAL SOCIETY OF AMERICA 2000; ABSTRACTS OF THE 95TH ANNUAL MEETING Ver registro
7.- REGIONAL VARIATIONS OF SEISMIC ATTENUATION OF LG WAVES IN SOUTHERN MEXICO AMERICAN GEOPHYSICAL UNION; WASHINGTON, DC; USA; UNITED STATES, 1997 Ver registro
8.- Remote triggered seismicity caused by the 2011, M9.0 Tohoku-Oki, Japan earthquake American Geophysical Union; Washington, DC; USA; United States, 2012 Ver registro
9.- S WAVE ATTENUATION IN THE COASTAL REGION OF JALISCO-COLIMA, MEXICO ELSEVIER; AMSTERDAM; NLD; NETHERLANDS, 1999 Ver registro
10.- Seismic anisotropy in northern and central Gulf of California region, Mexico, from teleseismic receiver functions and new evidence of possible plate capture American Geophysical Union; Washington, DC; USA; United States, 2008 Ver registro
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