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dc.contributor.authorOviedo Prada, Karem
dc.contributor.authorMuñoz Pérez, Juan José 
dc.contributor.authorEscobar Olaya, Germán A.
dc.contributor.authorOsorio-Granada, Ana Maria
dc.contributor.authorHowden, Stephan
dc.contributor.authorTorrecillas Lozano, Cristina
dc.contributor.authorRomero Cózar, Jeanette 
dc.contributor.authorContreras de Villar, Antonio 
dc.contributor.authorLeón-Rincón, Hermann
dc.contributor.authorJigena Antelo, Bismarck 
dc.contributor.otherCiencias y Técnicas de la Navegación y Construcciones Navaleses_ES
dc.contributor.otherFísica Aplicadaes_ES
dc.contributor.otherIngeniería Industrial e Ingeniería Civiles_ES
dc.date.accessioned2024-03-13T07:59:00Z
dc.date.available2024-03-13T07:59:00Z
dc.date.issued2024-03
dc.identifier.issn1010-6049
dc.identifier.urihttp://hdl.handle.net/10498/31372
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 inter-pretation. We could then characterise the submarine relief, ana-lyse 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 500m, 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 dir-ect relationship between the magnetic anomalies and bathymetry of the seafloor was confirmed, reinforcing the theory of the vol-canic origin of these islandses_ES
dc.formatapplication/pdfes_ES
dc.language.isoenges_ES
dc.publisherTaylor and Francises_ES
dc.sourceGeocarto International, 39:1es_ES
dc.subjectASPSCes_ES
dc.subjectColombian Caribbean Seaes_ES
dc.subjectbathymetriees_ES
dc.subjectmagnetic anomalieses_ES
dc.subjectmarine geophysicses_ES
dc.titleResults of high-resolution technologies applied in the acquisition of seafloor information in the Colombian Caribbean Seaes_ES
dc.typejournal articlees_ES
dc.rights.accessRightsopen accesses_ES
dc.identifier.doi10.1080/10106049.2024.2321365
dc.type.hasVersionVoRes_ES


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