Estudio combinado paleomagnético y petromagnético de flujos de lava asociados al rift Tepic-Zacoalco emitidos durante los crhones geomagnéticos Gauss y Gilbert
Instituto de Investigaciones en Ciencias de la Tierra. Maestría en Geociencias y Planificación del Territorio Using paleomagnetique techniques it was possible to determine 17 directions from a total of 21 study sites, of which 4 have normal polarity, 8 reverse polarity and 5 intermediate polarities,...
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Universidad Michoacana de San Nicolás de Hidalgo
2019
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Online Access: | http://bibliotecavirtual.dgb.umich.mx:8083/xmlui/handle/DGB_UMICH/4429 |
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ftunivmichoacana:oai:bibliotecavirtual.dgb.umich.mx:DGB_UMICH/4429 2023-05-15T16:19:41+02:00 Estudio combinado paleomagnético y petromagnético de flujos de lava asociados al rift Tepic-Zacoalco emitidos durante los crhones geomagnéticos Gauss y Gilbert Ulises Demian Díaz Ortega Mikhail Ostrooumov Avtandil Gogichaishvili 2019-07 application/pdf http://bibliotecavirtual.dgb.umich.mx:8083/xmlui/handle/DGB_UMICH/4429 spa spa Universidad Michoacana de San Nicolás de Hidalgo http://bibliotecavirtual.dgb.umich.mx:8083/xmlui/handle/DGB_UMICH/4429 info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by-nc-nd/4.0 CC-BY-NC-ND info:eu-repo/classification/cti/1 INICIT-M-2019-0985 Paleopolos Ritf Tectónica info:eu-repo/semantics/masterThesis 2019 ftunivmichoacana 2022-06-13T07:02:58Z Instituto de Investigaciones en Ciencias de la Tierra. Maestría en Geociencias y Planificación del Territorio Using paleomagnetique techniques it was possible to determine 17 directions from a total of 21 study sites, of which 4 have normal polarity, 8 reverse polarity and 5 intermediate polarities, the last ones have a cone of certainty that ranges from 2.5 to 22°. The samples come from lava flows located along the Tepic-Zacoalco Rift. Which have high quality radiometric tests that reportages between 3 and 5Ma. Rock magnetism tests were performed which allow to obtain the variability of magnetic susceptibility as a function of temperature (kT curves), most of the samples have a single phase close to 570 ° C which is representative of poor in titanium titanomagnetite. In the case of sites that have two phases, the first one is located around 360 ° C, while the second and dominant phase is approximately 560 ° C which is consistent with titanomagnetite with high and low content in titanium. By discarding the intermediate polarities and inverting the reverse polarities, it was possible to calculate the paleomagnetic average with Dec = 347.4 °, Inc = 29.2 °, N = 12, α95 = 9.7 °. The position of virtual geomagnetic pole the obtained is PLat = 77.9 ° N, PLong = 160.3 ° E, A95 = 6.83 °, N = 21. Comparing the pole obtained with the apparent polar drift curves for North America (APWP) published by Besse and Courtillot (2002) and Torsvik et al., (2008) which were calculated for a 5Ma window, a significant difference is observed, which can be attributed to a possible independent displacement of the Jalisco Block with respect to the North American plate. Considering the radiometric ages of each sample and the determined polarity, it was possible to construct a column of geomagnetic polarities. Mediante técnicas paleomagnéticas fue posible determinar 17 direcciones de un total de 21sitios de estudio, de las cuales 4 tienen una polaridad normal, 8 polaridad invertida y 5 con polaridades intermedias, de estas últimas ... Master Thesis Geomagnetic Pole Repositorio Institucional de la Universidad Michoacana de San Nicolás de Hidalgo (DSpace) |
institution |
Open Polar |
collection |
Repositorio Institucional de la Universidad Michoacana de San Nicolás de Hidalgo (DSpace) |
op_collection_id |
ftunivmichoacana |
language |
Spanish |
topic |
info:eu-repo/classification/cti/1 INICIT-M-2019-0985 Paleopolos Ritf Tectónica |
spellingShingle |
info:eu-repo/classification/cti/1 INICIT-M-2019-0985 Paleopolos Ritf Tectónica Ulises Demian Díaz Ortega Estudio combinado paleomagnético y petromagnético de flujos de lava asociados al rift Tepic-Zacoalco emitidos durante los crhones geomagnéticos Gauss y Gilbert |
topic_facet |
info:eu-repo/classification/cti/1 INICIT-M-2019-0985 Paleopolos Ritf Tectónica |
description |
Instituto de Investigaciones en Ciencias de la Tierra. Maestría en Geociencias y Planificación del Territorio Using paleomagnetique techniques it was possible to determine 17 directions from a total of 21 study sites, of which 4 have normal polarity, 8 reverse polarity and 5 intermediate polarities, the last ones have a cone of certainty that ranges from 2.5 to 22°. The samples come from lava flows located along the Tepic-Zacoalco Rift. Which have high quality radiometric tests that reportages between 3 and 5Ma. Rock magnetism tests were performed which allow to obtain the variability of magnetic susceptibility as a function of temperature (kT curves), most of the samples have a single phase close to 570 ° C which is representative of poor in titanium titanomagnetite. In the case of sites that have two phases, the first one is located around 360 ° C, while the second and dominant phase is approximately 560 ° C which is consistent with titanomagnetite with high and low content in titanium. By discarding the intermediate polarities and inverting the reverse polarities, it was possible to calculate the paleomagnetic average with Dec = 347.4 °, Inc = 29.2 °, N = 12, α95 = 9.7 °. The position of virtual geomagnetic pole the obtained is PLat = 77.9 ° N, PLong = 160.3 ° E, A95 = 6.83 °, N = 21. Comparing the pole obtained with the apparent polar drift curves for North America (APWP) published by Besse and Courtillot (2002) and Torsvik et al., (2008) which were calculated for a 5Ma window, a significant difference is observed, which can be attributed to a possible independent displacement of the Jalisco Block with respect to the North American plate. Considering the radiometric ages of each sample and the determined polarity, it was possible to construct a column of geomagnetic polarities. Mediante técnicas paleomagnéticas fue posible determinar 17 direcciones de un total de 21sitios de estudio, de las cuales 4 tienen una polaridad normal, 8 polaridad invertida y 5 con polaridades intermedias, de estas últimas ... |
author2 |
Mikhail Ostrooumov Avtandil Gogichaishvili |
format |
Master Thesis |
author |
Ulises Demian Díaz Ortega |
author_facet |
Ulises Demian Díaz Ortega |
author_sort |
Ulises Demian Díaz Ortega |
title |
Estudio combinado paleomagnético y petromagnético de flujos de lava asociados al rift Tepic-Zacoalco emitidos durante los crhones geomagnéticos Gauss y Gilbert |
title_short |
Estudio combinado paleomagnético y petromagnético de flujos de lava asociados al rift Tepic-Zacoalco emitidos durante los crhones geomagnéticos Gauss y Gilbert |
title_full |
Estudio combinado paleomagnético y petromagnético de flujos de lava asociados al rift Tepic-Zacoalco emitidos durante los crhones geomagnéticos Gauss y Gilbert |
title_fullStr |
Estudio combinado paleomagnético y petromagnético de flujos de lava asociados al rift Tepic-Zacoalco emitidos durante los crhones geomagnéticos Gauss y Gilbert |
title_full_unstemmed |
Estudio combinado paleomagnético y petromagnético de flujos de lava asociados al rift Tepic-Zacoalco emitidos durante los crhones geomagnéticos Gauss y Gilbert |
title_sort |
estudio combinado paleomagnético y petromagnético de flujos de lava asociados al rift tepic-zacoalco emitidos durante los crhones geomagnéticos gauss y gilbert |
publisher |
Universidad Michoacana de San Nicolás de Hidalgo |
publishDate |
2019 |
url |
http://bibliotecavirtual.dgb.umich.mx:8083/xmlui/handle/DGB_UMICH/4429 |
genre |
Geomagnetic Pole |
genre_facet |
Geomagnetic Pole |
op_relation |
http://bibliotecavirtual.dgb.umich.mx:8083/xmlui/handle/DGB_UMICH/4429 |
op_rights |
info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by-nc-nd/4.0 |
op_rightsnorm |
CC-BY-NC-ND |
_version_ |
1766006101941157888 |