Registros del 1 al 8 de 8 encontrados |
![](./images/clear.gif) 1.- EVIDENCE FOR ACTIVE EXTENSIONAL TECTONIC FEATURES WITHIN THE ACAPULCO TRENCH FILL AT THE RIVERA-NORTH AMERICA PLATE BOUNDARY
GAUTHIER-VILLARS; MONTROUGE; FRA; FRANCE, 1996
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![](./images/clear.gif) 2.- GEOCHEMISTRY OF THE MABUJINA COMPLEX, CENTRAL CUBA; IMPLICATIONS ON THE CUBAN CRETACEOUS ARC ROCKS
UNIVERSITY OF CHICAGO PRESS; CHICAGO, IL; USA; UNITED STATES, 2003
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![](./images/clear.gif) 3.- LARGE NEOGENE SUBSIDENCE EVENT ALONG THE MIDDLE AMERICA TRENCH OFF MEXICO (18 DEGREES -19 DEGREES N); EVIDENCE FROM SUBMERSIBLE OBSERVATIONS
GEOLOGICAL SOCIETY OF AMERICA (GSA); BOULDER, CO; USA; UNITED STATES, 1997
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![](./images/clear.gif) 4.- NEOGENE SUBSIDENCE EVENT ALONG THE ACAPULCO TRENCH OFF MANZANILLO (MEXICO, 18-19 DEGREES N); EVIDENCE FROM DEEP SEA SUBMERSIBLE OBSERVATIONS
AMERICAN GEOPHYSICAL UNION; WASHINGTON, DC; USA; UNITED STATES, 1995
AGU 1995 FALL MEETING
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![](./images/clear.gif) 5.- Preliminary report on aftershock recording and site characterization in Haiti
Seismological Society of America; El Cerrito, CA; USA; United States, 2010
The January/February 2010 earthquakes in Haiti, offshore Northern California, and Chile; origins, impacts and lessons learned; abstracts
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![](./images/clear.gif) 6.- STRIKE-SLIP TECTONICS AND SEISMICITY ALONG THE NORTHERN CARIBBEAN PLATE BOUNDARY FROM CUBA TO HISPANIOLA
GEOLOGICAL SOCIETY OF AMERICA (GSA); BOULDER, CO; USA; UNITED STATES, 1998
ACTIVE STRIKE-SLIP AND COLLISIONAL TECTONICS OF THE NORTHERN CARIBBEAN PLATE BOUNDARY ZONE
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![](./images/clear.gif) 7.- THE LATE CRETACEOUS DUARTE COMPLEX AND SIETE CABEZAS FORMATION (HISPANIOLA); CARIBBEAN OCEANIC PLATEAU
MINERALOGICAL SOCIETY; LONDON; GBR; UNITED KINGDOM, 1998
V. M. GOLDSCHMIDT CONFERENCE; EXTENDED ABSTRACTS
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![](./images/clear.gif) 8.- The tsunami of Djidjelli (eastern Algeria) of August 22nd, 1856; the seismotectonic context and its modelling
IUGG; [location varies]; III; International, 2007
Earth; our changing planet; proceedings of IUGG XXIV general assembly
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