Modeling the crust and upper mantle in northern Beata Ridge (CARIBE NORTE Project)

dc.contributor.authorNúñez Escribano, Diana
dc.contributor.authorCórdoba Barba, Diego
dc.contributor.authorCotilla Rodríguez, Mario Octavio
dc.contributor.authorPazos, Antonio
dc.date.accessioned2024-02-06T17:04:59Z
dc.date.available2024-02-06T17:04:59Z
dc.date.issued2015-10-18
dc.description.abstractThe complex tectonic region of NE Caribbean, where Hispaniola and Puerto Rico are located, is bordered by subduction zone with oblique convergence in the north and by incipient subduction zone associated to Muertos Trough in the south. Central Caribbean basin is characterized by the presence of a prominent topographic structure known as Beata Ridge, whose oceanic crustal thickness is unusual. The northern part of Beata Ridge is colliding with the central part of Hispaniola along a transverse NE alignment, which constitutes a morphostructural limit, thus producing the interruption of the Cibao Valley and the divergence of the rivers and basins in opposite directions. The direction of this alignment coincides with the discontinuity that could explain the extreme difference between west and east seismicity of the island. Different studies have provided information about Beata Ridge, mainly about the shallow structure from MCS data. In this work, CARIBE NORTE (2009) wide-angle seismic data are analyzed along a WNW-ESE trending line in the northern flank of Beata Ridge, providing a complete tectonic view about shallow, middle and deep structures. The results show clear tectonic differences between west and east separated by Beata Island. In the Haiti Basin area, sedimentary cover is strongly influenced by the bathymetry and its thickness decreases toward to the island. In this area, the Upper Mantle reaches 20 km deep increasing up to 24 km below the island where the sedimentary cover disappears. To the east, the three seamounts of Beata Ridge provoke the appearance of a structure completely different where sedimentary cover reaches thicknesses of 4 km between seamounts and Moho rises up to 13 km deep. This study has allowed to determine the Moho topography and to characterize seismically the first upper mantle layers along the northern Beata Ridge, which had not been possible with previous MCS data.
dc.description.departmentDepto. de Física de la Tierra y Astrofísica
dc.description.facultyFac. de Ciencias Físicas
dc.description.refereedTRUE
dc.description.sponsorshipMinisterio de Educación y Ciencia (España)
dc.description.statuspub
dc.identifier.citationNúñez, D., Córdoba, D., Cotilla, M.O. et al. Modeling the Crust and Upper Mantle in Northern Beata Ridge (CARIBE NORTE Project). Pure Appl. Geophys. 173, 1639–1661 (2016). https://doi.org/10.1007/s00024-015-1180-0
dc.identifier.doi10.1007/s00024-015-1180-0
dc.identifier.essn1420-9136
dc.identifier.issn0033-4553
dc.identifier.officialurlhttps://link.springer.com/article/10.1007/s00024-015-1180-0
dc.identifier.urihttps://hdl.handle.net/20.500.14352/99656
dc.issue.number5
dc.journal.titlePure and Applied Geophysics
dc.language.isoeng
dc.page.final1661
dc.page.initial1639
dc.publisherSpringer
dc.relation.projectIDinfo:eu-repo/grantAgreement/MEC//CTM2006-13666-C02-02/ES/ANALISIS DEL CONTACTO ENTRE LAS PLACAS CARIBE Y NORTEAMERICANA: DESDE LA CRESTA DE BEATA (R. DOMINICANA) HASTA EL PASAJE DE ANEGADA (ANTILLAS MENORES): CARIBE NORTE/
dc.relation.projectIDCTM2008-02955-E/MAR
dc.relation.projectIDinfo:eu-repo/grantAgreement/MICINN//CGL2011-29474-C02-01/ES/CARACTERIZACION DEL PELIGRO SISMICO Y TSUNAMIGENICO ASOCIADO CON LA ESTRUCTURA CORTICAL DEL CONTACTO PLACA DE RIVERA-BLOQUE DE JALISCO (REFRACCION%2FSISMICIDAD)/
dc.rights.accessRightsrestricted access
dc.subject.cdu550.3
dc.subject.keywordBeata Ridge
dc.subject.keywordCaribbean plate
dc.subject.keywordHispaniola
dc.subject.keywordShallow and deep structures
dc.subject.keywordWide-angle seismics
dc.subject.ucmGeofísica
dc.subject.unesco2507.05 Sismología y Prospección Sísmica
dc.titleModeling the crust and upper mantle in northern Beata Ridge (CARIBE NORTE Project)
dc.typejournal article
dc.type.hasVersionAM
dc.volume.number173
dspace.entity.typePublication
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relation.isAuthorOfPublication.latestForDiscovery358a1128-ccfa-47b6-b29f-f17ef7a90316
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