Registros del 1 al 4 de 4 encontrados |
![](./images/clear.gif) 1.- ARE THE REGIONAL VARIATIONS IN CENTRAL AMERICAN ARC LAVAS DUE TO DIFFERING BASALTIC VERSUS PERIDOTITIC SLAB SOURCES OF FLUIDS?
GEOLOGICAL SOCIETY OF AMERICA (GSA); BOULDER, CO; USA; UNITED STATES, 2002
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![](./images/clear.gif) 2.- Horizontal asthenosphere flow beneath the lithosphere
Copernicus GmbH on behalf of the European Geosciences Union (EGU); Katlenburg-Lindau; DEU; Germany, 2010
European Geosciences Union general assembly 2010
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![](./images/clear.gif) 3.- LINKS BETWEEN FAULTING OF THE INCOMING OCEAN PLATE AND EARTHQUAKES IN THE SLAB OF SUBDUCTION ZONES
AMERICAN GEOPHYSICAL UNION; WASHINGTON, DC; USA; UNITED STATES, 2002
AGU 2002 FALL MEETING
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![](./images/clear.gif) 4.- Tectonic structure of the Middle America Pacific margin and incoming Cocos Plate from Costa Rica to Guatemala
American Geophysical Union; Washington, DC; USA; United States, 2003
AGU 2003 fall meeting
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