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dc.creatorOviedo Prada, Karemes
dc.creatorMuñoz Pérez, Juan Josées
dc.creatorEscobar Olaya, Germánes
dc.creatorOsorio Granada, Ana Maríaes
dc.creatorHowden, Stephanes
dc.creatorTorrecillas Lozano, Cristinaes
dc.creatorRomero Cózar, Jeanettees
dc.creatorContreras de Villar, Antonioes
dc.creatorLeón Rincón, Hermannes
dc.creatorJigena Antelo, Bismarckes
dc.date.accessioned2024-05-21T09:38:48Z
dc.date.available2024-05-21T09:38:48Z
dc.date.issued2024
dc.identifier.citationOviedo Prada, K., Muñoz Pérez, J.J., Escobar Olaya, G., Osorio Granada, A.M., Howden, S., Torrecillas Lozano, C.,...,Jigena Antelo, B. (2024). Results of high-resolution technologies applied in the acquisition of seafloor information in the Colombian Caribbean Sea. Geocarto International, 39(1) (2321365). https://doi.org/10.1080/10106049.2024.2321365.
dc.identifier.issn1010-6049es
dc.identifier.issn1752-0762es
dc.identifier.urihttps://hdl.handle.net/11441/158726
dc.description.abstractWe expound on a hydrographic and geophysical survey in the south of the Archipelago of San Andres, Providencia, and Santa Catalina (ASAPSC) in the Colombian Caribbean Sea. In 2017 and 2018, high-resolution data were acquired from the Caribbean Center for Oceanographic and Hydrographic Research (CIOH). The hydrographic data were processed and filtered per International Hydrographic Organization (IHO) standards and the geomagnetic data were processed, corrected, and filtered to improve the interpretation. We could then characterise the submarine relief, analyse the geomagnetic anomalies in the area, and identify different relief forms of volcanic origin. Regarding geomagnetic work, a spectral analysis of the anomalies revealed highly magnetic bodies in deep water and residual magnetic anomalies strongly related to the seabed morphology. Magnetic highs associated with the basement highs and volcanic cones were detected. Complementary spectral analysis showed that the shallowest magnetic sources were in the first 500 m, whereas the deepest magnetic sources were between the depths of 4 and 5 km. The geomagnetic data were also validated using Euler deconvolution analysis, which confirmed these magnetic anomalies. Thus, a direct relationship between the magnetic anomalies and bathymetry of the seafloor was confirmed, reinforcing the theory of the volcanic origin of these islands.es
dc.formatapplication/pdfes
dc.format.extent21 p.es
dc.language.isoenges
dc.publisherTaylor and Francises
dc.relation.ispartofGeocarto International, 39(1) (2321365).
dc.rightsAtribución-NoComercial 4.0 Internacional*
dc.rights.urihttp://creativecommons.org/licenses/by-nc/4.0/*
dc.subjectColombian Caribbean Seaes
dc.subjectASPSCes
dc.subjectBathymetryes
dc.subjectMagnetic anomalieses
dc.subjectMarine geo-physicses
dc.titleResults of high-resolution technologies applied in the acquisition of seafloor information in the Colombian Caribbean Seaes
dc.typeinfo:eu-repo/semantics/articlees
dc.type.versioninfo:eu-repo/semantics/publishedVersiones
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses
dc.contributor.affiliationUniversidad de Sevilla. Departamento de Ingeniería Gráficaes
dc.relation.projectIDRNM912es
dc.relation.publisherversionhttps://www.tandfonline.com/doi/full/10.1080/10106049.2024.2321365es
dc.identifier.doi10.1080/10106049.2024.2321365es
dc.contributor.groupUniversidad de Sevilla. RNM931: Tecnologías de la Información Geoespacial, Gráfica e Hidrológicaes
dc.journaltitleGeocarto Internationales
dc.publication.volumen39(1)es
dc.publication.issue2321365es
dc.contributor.funderUniversidad de Cádizes

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