Please use this identifier to cite or link to this item: https://cir.cenieh.es/handle/20.500.12136/2993
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dc.contributor.authorEscuder-Viruete, Javier-
dc.contributor.authorFernández Rodríguez, Francisco José-
dc.contributor.authorPérez Valera, Fernando-
dc.contributor.authorMedialdea, Alicia-
dc.date.accessioned2023-06-01T11:34:15Z-
dc.date.issued2023-
dc.identifier.citationDigital CSIC, 2023 [Dataset]es_ES
dc.identifier.urihttps://cir.cenieh.es/handle/20.500.12136/2993-
dc.description.abstractThis dataset present methodological, seismic, structural and geochronological (optically stimulated luminescence) data collected in southern central Hispaniola Island to better understand the regional process of collision between the Beata Ridge and the back-arc margin of the Caribbean island-arc. In particular, the role played by the Ocoa-Bonao-La Guacara fault zone (OBGFZ), which is an active, NNE to NE-striking large-scale fault system that crosses the southern central sector of Hispaniola in the Dominican Republic along more than 250 km.es_ES
dc.description.sponsorshipThe research was funded through PID2019-105625RB-C22 project of the 940 MCIN/AEI/10.13039/501100011033 of the Spanish Governmentes_ES
dc.language.isoenes_ES
dc.publisherDIGITAL.CSICes_ES
dc.rightsinfo:eu-repo/semantics/openAccesses_ES
dc.rightsAttribution-NonCommercial-NoDerivatives 4.0 International (CC BY-NC-ND 4.0)*
dc.rights.urihttps://creativecommons.org/licenses/by-nc-nd/4.0/*
dc.titleDataset for Present-day accommodation of Caribbean-North American oblique plate convergence through the Ocoa-Bonao-La Guacara fault zone, southern central Hispaniola: a transition zone between oceanic subduction and arc-oceanic plateau collisiones_ES
dc.typeDatasetes_ES
dc.identifier.doi10.20350/DIGITALCSIC/15220-
dc.relation.publisherversionhttps://doi.org/10.20350/DIGITALCSIC/15220es_ES
dc.date.available2023-06-01T11:34:15Z-
Appears in Collections:Geocronología y Geología

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