3D analytical signal application in magnetic marine data processing for a shipwreck in the Colombian Caribbean
DOI:
https://doi.org/10.26640/22159045.207Keywords:
Magnetic anomalies, analytic signal, magnetometer, shipwreckAbstract
On a cruise for magnetic data gathering, aboard the ship A.R.C “Providencia” the magnetic and bathymetric survey was carried out simultaneously within the area delimited by the geographic coordinates 10°20'50” N - 10°21'30” N latitude and 75°35'40” W- 75°36'20” W longitude, close to the Tierra Bomba island. Given the shipwreck Ex A.R.C “Pedro de Heredia” high magnetic susceptibility and with the purpose of identifying its anomalous response, two research areas were designed, a general one and a detailed one, covering an area of 2.25 km with 22 lines separated 50 m and an area of 20.08 km with 8 lines separated 20 m respectively in the North – South direction. This way, the first research cruise using the marine magnetometer Geometrics G-882 had taken place. Once the data had been gathered, the magnetic anomaly charts were obtained to which the corresponding corrections for daytime variation and regional anomaly to model IGRF 2005 were made. Since the purpose of the Research was to identify the anomaly source, in the data processing, the 3D analytical signal technique was used, for the values of the total magnetic field anomalies, whose results show accurately the location and depth of the shipwreck, showing that this method permits the identification of the magnetic source as well as discriminating it from other geo-forms obtained through bathymetry.Downloads
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References
[1] Briceño LA, Rey C, Hernandez O, Zamora J.A, New Magnetic Anomalies Map of Colombia. Earth Sciences Research Journal, 2008; 12:7-12.
[2] Larson T, Norris T. Champaign Magnetometer survey for buried steamboats near the mouth of the missouri river. Illinois State Geological Survey, ILUS and Army Corps of Engineers, [online] 2007. Disponible en internet: URLhttp://www.x-cdtech.com/SAGEEP08/pdfs/69.pdf.
[3] Wilde-Ramsing M, Arqueological Investgations at the Qeen Anne's Revenge Shipwreck Site. Research report and bulletin series QAR-R-09-03. Underwater Archaeology Branch. Office of State Archaeology. Department of Cultural Resources State of North Carolina. [online] 2009. Disponible en internet URL: http://www.qaronline.org/techSeries/QAR-R-09-03.pdf.
[4] Boyce J, Reinhardt E, Raban A, Pozza M. Marine Magnetic Survey of a Submerged Roman Harbour. The International Journal of Nautical Archaeology. 2004; 33.1: 122–136.
[5] Nabighian, M N, Toward the three-dimensional automatic interpretation of potential field data via generalized Hilbert transforms: Fundamental relations J. Geophysics, 1984; 53: 957-966.
[6] Roest, WE, Verhoef, J, Pilkington M. Magnetic interpretation using 3-D analytic signal. J. Geophysics, 1992; 57: 116-125.
[7] MacLeod I, Jones K, Dai T. 3-D Analytic Signal in the Interpretation of Total Magnetic Field Data at Low Magnetic Latitudes. Exploration Geophysics. 1993; 24: 679-688.
[8] Campbell WH. Introduction to Geomagnetic Fields, England: Cambridge University Press; 2003.
[9] Rodríguez D M. Modelo de la Falla de Soapaga a partir de la Correlación Espectral de Campos Potenciales. Tesis Maestría en Ciencias – Geofísica. Universidad Nacional de Colombia. Bogotá, Colombia; 2008.
[10] Mandea M and Macmillan S. International Geomagnetic Reference Field—the eighth generation. Earth Planets Space., 2000; 52: 1119–1124.
[11] Lertxundi A. Métodos de Estadística Espacial para evaluar la Influencia de Factores Medio Ambientales sobre la Incidencia y Mortalidad por Cáncer. Tesis, Universidad de Girona. Girona, España; 2006. Disponible en internet: URLhttp://www.tdr.cesca.es/TESIS_UdG/AVAILABLE/TDX-0313107-114758//talm.pdf.
[12] Fabra Camacho LM, Tellez Moncada S A. Determinación de la Anomalía Magnética Marina para una zona piloto de estudio en el Caribe colombiano. Trabajo de Ingeniería Catastral y Geodesia, Universidad Distrital Francisco José de Caldas. Bogotá, Colombia; 2009.
[13] Gómez F & Sandoval J. Estudio Geofísico Integrado en la Zona Yumare - Aroa, Estados Yaracuy y Falcón. Trabajo de Grado de Ingeniería Geofísica, Universidad Central de Venezuela. Caracas, Venezuela; 2008.
[14] Nabighian, M N. The analytic signal of two-dimensional magnetic bodies with polygonal crosssection: Its properties and use for automated anomaly interpretation. J. Geophysics, 1972; 37: 507-517.
[15] Nabighian, M N. Additional comments on the analytic signal of two-dimensional magnetic bodies with polygonal cross-section, J. Geophysics, 1974; 39:85-92.
[16] Keating P, Sailhac P. Use of the analytic signal to identify magnetic anomalies due to kimberlite pipes. J. Geophysics, 2004; 69: 180–190.
[17] Phillips D J. Locating magnetic contacts: a comparison of the horizontal gradient, analytic signal, and local wavenumber methods. [online] 2000. Disponible en internet: URL ftp://ftpext.usgs.gov/pub/cr/co/denver/musette/pub/
outside_pubs/jeff/Phillips_SEG2000.pdf.
[2] Larson T, Norris T. Champaign Magnetometer survey for buried steamboats near the mouth of the missouri river. Illinois State Geological Survey, ILUS and Army Corps of Engineers, [online] 2007. Disponible en internet: URLhttp://www.x-cdtech.com/SAGEEP08/pdfs/69.pdf.
[3] Wilde-Ramsing M, Arqueological Investgations at the Qeen Anne's Revenge Shipwreck Site. Research report and bulletin series QAR-R-09-03. Underwater Archaeology Branch. Office of State Archaeology. Department of Cultural Resources State of North Carolina. [online] 2009. Disponible en internet URL: http://www.qaronline.org/techSeries/QAR-R-09-03.pdf.
[4] Boyce J, Reinhardt E, Raban A, Pozza M. Marine Magnetic Survey of a Submerged Roman Harbour. The International Journal of Nautical Archaeology. 2004; 33.1: 122–136.
[5] Nabighian, M N, Toward the three-dimensional automatic interpretation of potential field data via generalized Hilbert transforms: Fundamental relations J. Geophysics, 1984; 53: 957-966.
[6] Roest, WE, Verhoef, J, Pilkington M. Magnetic interpretation using 3-D analytic signal. J. Geophysics, 1992; 57: 116-125.
[7] MacLeod I, Jones K, Dai T. 3-D Analytic Signal in the Interpretation of Total Magnetic Field Data at Low Magnetic Latitudes. Exploration Geophysics. 1993; 24: 679-688.
[8] Campbell WH. Introduction to Geomagnetic Fields, England: Cambridge University Press; 2003.
[9] Rodríguez D M. Modelo de la Falla de Soapaga a partir de la Correlación Espectral de Campos Potenciales. Tesis Maestría en Ciencias – Geofísica. Universidad Nacional de Colombia. Bogotá, Colombia; 2008.
[10] Mandea M and Macmillan S. International Geomagnetic Reference Field—the eighth generation. Earth Planets Space., 2000; 52: 1119–1124.
[11] Lertxundi A. Métodos de Estadística Espacial para evaluar la Influencia de Factores Medio Ambientales sobre la Incidencia y Mortalidad por Cáncer. Tesis, Universidad de Girona. Girona, España; 2006. Disponible en internet: URLhttp://www.tdr.cesca.es/TESIS_UdG/AVAILABLE/TDX-0313107-114758//talm.pdf.
[12] Fabra Camacho LM, Tellez Moncada S A. Determinación de la Anomalía Magnética Marina para una zona piloto de estudio en el Caribe colombiano. Trabajo de Ingeniería Catastral y Geodesia, Universidad Distrital Francisco José de Caldas. Bogotá, Colombia; 2009.
[13] Gómez F & Sandoval J. Estudio Geofísico Integrado en la Zona Yumare - Aroa, Estados Yaracuy y Falcón. Trabajo de Grado de Ingeniería Geofísica, Universidad Central de Venezuela. Caracas, Venezuela; 2008.
[14] Nabighian, M N. The analytic signal of two-dimensional magnetic bodies with polygonal crosssection: Its properties and use for automated anomaly interpretation. J. Geophysics, 1972; 37: 507-517.
[15] Nabighian, M N. Additional comments on the analytic signal of two-dimensional magnetic bodies with polygonal cross-section, J. Geophysics, 1974; 39:85-92.
[16] Keating P, Sailhac P. Use of the analytic signal to identify magnetic anomalies due to kimberlite pipes. J. Geophysics, 2004; 69: 180–190.
[17] Phillips D J. Locating magnetic contacts: a comparison of the horizontal gradient, analytic signal, and local wavenumber methods. [online] 2000. Disponible en internet: URL ftp://ftpext.usgs.gov/pub/cr/co/denver/musette/pub/
outside_pubs/jeff/Phillips_SEG2000.pdf.
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Published
2009-12-05
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RESEARCH ARTICLE
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How to Cite
3D analytical signal application in magnetic marine data processing for a shipwreck in the Colombian Caribbean. (2009). CIOH Scientific Bulletin, 27, 145-155. https://doi.org/10.26640/22159045.207
