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dc.creatorLücke Castro, Oscar H.
dc.creatorArroyo Hidalgo, Ivonne Gabriela
dc.date.accessioned2018-11-27T15:28:01Z
dc.date.available2018-11-27T15:28:01Z
dc.date.issued2015-10-29
dc.identifier.citationhttps://www.solid-earth.net/6/1169/2015/es_ES
dc.identifier.issn1869-9529
dc.identifier.urihttp://hdl.handle.net/10669/76181
dc.description.abstractThe eastern part of the oceanic Cocos Plate presents a heterogeneous crustal structure due to diverse origins and ages as well as plate-hot spot interactions which originated the Cocos Ridge, a structure that converges with the Caribbean Plate in southeastern Costa Rica. The complex structure of the oceanic plate directly influences the dynamics and geometry of the subduction zone along the Middle American Trench. In this paper an integrated interpretation of the slab geometry in Costa Rica is presented based on 3-D density modeling of combined satellite and surface gravity data, constrained by available geophysical and geological data and seismological information obtained from local networks. The results show the continuation of steep subduction geometry from the Nicaraguan margin into northwestern Costa Rica, followed by a moderate dipping slab under the Central Cordillera toward the end of the Central American Volcanic Arc. Contrary to commonly assumed, to the southeast end of the volcanic arc, our preferred model shows a steep, coherent slab that extends up to the landward projection of the Panama Fracture Zone. Overall, a gradual change in the depth of the intraplate seismicity is observed, reaching 220 km in the northwestern part, and becoming progressively shallower toward the southeast, where it reaches a maximum depth of 75 km. The changes in the terminal depth of the observed seismicity correlate with the increased density in the modeled slab. The absence of intermediate depth (> 75 km) intraplate seismicity in the southeastern section and the higher densities for the subducted slab in this area, support a model in which dehydration reactions in the subducted slab cease at a shallower depth, originating an anhydrous and thus aseismic slab.es_ES
dc.description.sponsorshipGerman Academic Exchange Service//DAAD/Alemaniaes_ES
dc.description.sponsorshipSpecial Priority Program 1257 “Mass Transport and Mass Distribution in the Earth System” of the German Research Foundation//DFG/Alemaniaes_ES
dc.language.isoen_USes_ES
dc.sourceSolid Earth, 6, 1169-1183, 2015es_ES
dc.subjectSubductiones_ES
dc.subjectTectonicses_ES
dc.subjectGravityes_ES
dc.subjectDensityes_ES
dc.subjectSeismologyes_ES
dc.subjectGeophysicses_ES
dc.titleDensity structure and geometry of the Costa Rican subduction zone from 3-D gravity modeling and local earthquake dataes_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.identifier.doi10.5194/se-6-1169-2015
dc.description.procedenceUCR::Vicerrectoría de Docencia::Ciencias Básicas::Facultad de Ciencias::Escuela Centroamericana de Geologíaes_ES


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