| Registros del 1 al 6 de 6 encontrados |
1.- ARE RUPTURE ZONE LIMITS OF GREAT SUBDUCTION EARTHQUAKES CONTROLLED BY UPPER PLATE STRUCTURES? EVIDENCE FROM MULTICHANNEL SEISMIC REFLECTION DATA ACQUIRED ACROSS THE NORTHERN ECUADOR; SOUTHWEST COLOMBIA MARGIN
AMERICAN GEOPHYSICAL UNION; WASHINGTON, DC; USA; UNITED STATES, 2004
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2.- DEEP STRUCTURES OF THE ECUADOR CONVERGENT MARGIN AND THE CARNEGIE RIDGE, POSSIBLE CONSEQUENCE ON GREAT EARTHQUAKES RECURRENCE INTERVAL
AMERICAN GEOPHYSICAL UNION; WASHINGTON, DC; USA; UNITED STATES, 2004
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3.- FIELDS OF MULTI-KILOMETER SCALE SUB-CIRCULAR DEPRESSIONS IN THE CARNEGIE RIDGE SEDIMENTARY BLANKET; EFFECT OF UNDERWATER CARBONATE DISSOLUTION?
ELSEVIER; AMSTERDAM; NLD; NETHERLANDS, 2005
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4.- Results from the NEAREST-SEIS deep seismic cruise across the Gulf of Cadiz accretionary wedge
American Geophysical Union; Washington, DC; USA; United States, 2009
AGU 2009 fall meeting
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5.- Seismic evidence for the presence of Jurassic oceanic crust in the central Gulf of Cadiz (SW Iberian margin)
Elsevier; Amsterdam; NLD; Netherlands, 2011
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6.- The 2010 Haiti earthquake; a complex fault pattern constrained by seismologic and tectonic observations
American Geophysical Union; Washington, DC; USA; United States, 2011
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