Conferencias
URI permanente para esta colecciónhttp://10.0.96.45:4000/handle/11056/18051
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Ítem Active Subduction on Both Coasts of Costa Rica Does not Represent an Important Tsunami Hazard(2007-05-22) Protti, Marino; González, V.Ítem Along-Arc Variations in Attenuation in the Nicaragua-Costa Rica Mantle Wedge(2006) Rychert, Catherine; Fischer, K. M.; Abers, G. A.; Syracuse, E.; Protti, Marino; González Salas, V.; Strauch, WilfriedÍtem Arsenic in wells at the Guayabo Caldera in Northwest Costa Rica(International Association of Volcanology and Chemistry of the Earth's Interior, 2018-09) Martínez Cruz, María; Brenes-Navarro, Gilberto; Herrera-Murillo, JorgeThe Guayabo Caldera, a 14 km diameter volcanic depression with Miravalles volcano rising 2028 ma.s.l. in the norte astern side of so called, formed by repeated eruption sand multiple collapses which dis membered earlier volcanoes between 1.5 to 0.6 m.y.ago. The pyroclastic-flow sheets represent more than 30 km 3 of dacitict or hyolitic magma associated to crystal fractionation processes.Ítem Balanced cross sections of the active fila coste, a thrust belt: constraints on the inner forearc response to shallow subduction of the Cocos ridge(2005) Sitchler, Jason; Fischer, Donald; Gardner, Thomas; Protti, MarinoÍtem Combined GPS, EDM and triangulation surveys of the rapid downslope motion of the western flank of Arenal Volcano, Costa Rica(2011) Muller, Cyril; Del Potro, R.; Biggs, Juliet; Gottsmann, Joachim; Van der Laat, R.; Ebmeier, S. K.Here we present initial conclusions of a one year-long combined geodesy campaign on Arenal Volcano, in Costa Rica (2008-2009). Our data shows evidence for an active local tectonic surrounding, and a 7cm/yr displacement field of the western flank of the volcano edifice that is in general agreement with recent INSAR studies. The study shows that a rigorous combination of simultaneous GPS, EDM (Electronic Distance Measurements) and triangulation measurements provide a time-cost effective approach to volcanic monitoring.Ítem Connections between hyper-acid crater lakes and ank springs: New evidence from Rincón de la Vieja Volcano (Costa Rica) and implications for lahar hazard assessment(2014-09) Martínez Cruz, María; Van Bergen, M. J.; De Moor, J. Maarten; Saénz, W.Ítem Connections between hyper-acid crater lakes and ank springs: New evidence from Rincón de la Vieja Volcano (Costa Rica) and implications for lahar hazard assessment(2014-09) Martínez Cruz, María; Van Bergen, M. J.; Avard, Geoffroy; De Moor, J. Maarten; Saénz, W.Ítem Constraining Upper Plate Deformation in Nicaragua Through Delineation of the August 3, 2005 Mw 6.3 Strike Slip Earthquake Fault Plane(2006) French, S. W.; Warren, L. M.; Fischer, K. M.; Abers, G. A.; Strauch, Wilfried; Protti, Marino; González, V.Ítem Crustal Thickness of the Central American Arc(2007-06-18) Auger, Laura; Abers, Geoff; Syracuse, Ellen; Fischer, Karen; Strauch, Wilfried; Protti, Marino; González, VictorÍtem Crustal Thickness Variations Beneath the Central American Arc(2006) Auger, L. S.; Abers, G.; Fischer, K.; Protti, Marino; González, Victor; Strauch, WilfriedÍtem Imaging the Subduction Factory: The TUCAN Broadband Seismic Experiment in Central America(2002-04) Abers, G.; Fischer, K.; Syracuse, E.; Mackenzie, L.; Rychert, C.; Protti, Marino; González, V.; Strauch, WilfriedÍtem Mantle anisotropy beneath Costa Rica and Nicaragua and the TUCAN Broadband Seismometer Array(2004) Fischer, K. M.; Rychert, C. A.; Walker, A.; Abers, G. A.; Auger, L.; Syracuse, E.; Plank, T. A.; Protti, Marino; Salas, V. G.; Strauch, Wilfried; Perez, P.Ítem NICOYA, COSTA RICA, TRANS-PENINSULA GPS EXPERIMENT AND INTER-PLATE COUPLING(2003-06-30) Iinuma, Takeshi; Protti, Marino; Obana, Koichiro; Miyazaki, Shinichi; González, Victor; Van der Laat, Rodolfo; Kato, Teruyuki; Kaneda, Yoshiyuki; Hernández, EnriqueSince 2001, a GPS observation project has been carried out on the Nicoya Peninsula, Costa Rica. Costa Rica is located on the western margin of the Caribbean plate, and the Cocos plate is subducting under the Caribbean plate from the Mesoamerican Trench. The speed of convergence between the two plates has caused large earthquakes on the west coast of Costa Rica.Ítem Nicoya, Costa Rica: an IOPD target where the seismogenic zone or large earthquake can be drilled and instrumented(2009-09-23) Protti, Marino; González, Victor; Yoshiyuki, Kaneda; Brown, KevinÍtem Potential for the installation of a system in northern Costa Rica for early warning to the capital city of San Jose, from large subduction earthquakes under the Nicoya peninsula(1998-09-09) Protti, Marino; González, Victor; Malavassi, Eduardo; Hernández, Enrique; Guendel, FedericoÍtem Rayleigh Wave Tomography in the Nicaragua-Costa Rica Subduction Zone(2006) Salas de la Cruz, M.; Fischer, K. M.; Forsyth, D. W.; Abers, G. A.; Strauch, Wilfried; Protti, Marino; González, VictorÍtem Recovering the Importance of Monitoring Networks of Natural Processes in the Concept of Early Warning Systems(2003) Protti, Marino; González, VictorÍtem Recovering the Importance of Monitoring Networks of Natural Processes in the Concept of Early Warning Systems(2006) Protti, Marino; González, VictorÍtem Seismic and Geodetic Monitoring of the Nicoya, Costa Rica, Seismic Gap(2007-05-22) Protti, Marino; González, Victor; Schwartz, Susan; Timothy, Dixon; Kato, Teruyuki; Yoshiyuki, Kaneda; Simila, Gerald; SAMPSON, DANIELÍtem Seismic Velocities and Earthquake Locations in the Central America Upper Mantle: results from the TUCAN Experiment(2006) Syracuse, E. M.; Abers, G. A.; Auger, L.; Fischer, K.; Protti, Marino; González, Victor; Strauch, Wilfried; Brewer, J.