Paleomagnetic Pole Positions and Geomagnetic Secular Variation from the Cretaceous Ponta Grossa Dike Swarm (Brazil)
- Autores
- Cervantes Solano, Miguel; Goguitchaichvili, Avto; Mena, Mabel; Alva Valdivia, Luis; Morales Contreras, Juan; Cejudo Ruiz, Rubén; López Loera, Héctor; Soler, Ana María; Urrutia Fucugauchi, Jaime
- Año de publicación
- 2015
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- A detailed paleomagnetic and rock magnetic investigation has been carried out on the Early Cretaceous Ponta Grossa dike swarm in southern Brazil. This formation seems an excellent target for paleomagnetic study. The dikes are widely distributed over a large area, easy to access, and they record faithfully the geomagnetic field at the time of the eruption. Most of them are fresh and have been dated by K-Ar and Ar-Ar. Thermomagnetic experiments (low-field versus temperature curves) suggest low-Ti titanomagnetites as main remanence carriers, and their domain structure is characterised by a mixture of single-domain and multi-domain grains. Characteristic paleomagnetic directions are retrieved from 28 out of 29 sites (235 standard paleomagnetic cores). 17 sites show normal polarity, 10 sites show reverse polarity and one site shows an oblique direction, with negative inclination, separated 79° of the mean normal directions. The reversal test is positive at the 95% confidence level which ensures that the secondary remanent magnetizations were successfully removed and the sampling adequately averaged the palaeosecular variation. The paleosecular variation parameters values obtained in this study correlate with those determined for the Cretaceous Normal Superchron, between 125 to 84 Ma. The new paleomagnetic pole position (222.0° E, 88.1° S, N = 24, K = 35.68, A95 = 5.0°) agrees well (within uncertainties) with the reference poles determined from Besse and Courtillot (2002), and disagree with those reported in previous studies. The new results should be considered for estimating the Cretaceous paleomagnetic poles for stable South America.
Fil: Cervantes Solano, Miguel. Universidad Nacional Autónoma de México; México
Fil: Goguitchaichvili, Avto. Universidad Nacional Autónoma de México; México
Fil: Mena, Mabel. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geociencias Basicas, Aplicadas y Ambientales de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geociencias Basicas, Aplicadas y Ambientales de Buenos Aires; Argentina
Fil: Alva Valdivia, Luis. Instituto Potosino de Investigación Científica y Tecnológica; México
Fil: Morales Contreras, Juan. Universidad Nacional Autónoma de México; México
Fil: Cejudo Ruiz, Rubén. Universidad Nacional Autónoma de México; México
Fil: López Loera, Héctor. Instituto Potosino de Investigación Científica y Tecnológica; México
Fil: Soler, Ana María. Instituto Potosino de Investigación Científica y Tecnológica; México
Fil: Urrutia Fucugauchi, Jaime. Universidad Nacional Autónoma de México; México - Materia
-
Ponta Grossa Dike Swarm
South America
Paleomagnetism
Cretaceous - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- https://creativecommons.org/licenses/by-nc-nd/2.5/ar/
- Repositorio
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/20776
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Paleomagnetic Pole Positions and Geomagnetic Secular Variation from the Cretaceous Ponta Grossa Dike Swarm (Brazil)Cervantes Solano, MiguelGoguitchaichvili, AvtoMena, MabelAlva Valdivia, LuisMorales Contreras, JuanCejudo Ruiz, RubénLópez Loera, HéctorSoler, Ana MaríaUrrutia Fucugauchi, JaimePonta Grossa Dike SwarmSouth AmericaPaleomagnetismCretaceoushttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1A detailed paleomagnetic and rock magnetic investigation has been carried out on the Early Cretaceous Ponta Grossa dike swarm in southern Brazil. This formation seems an excellent target for paleomagnetic study. The dikes are widely distributed over a large area, easy to access, and they record faithfully the geomagnetic field at the time of the eruption. Most of them are fresh and have been dated by K-Ar and Ar-Ar. Thermomagnetic experiments (low-field versus temperature curves) suggest low-Ti titanomagnetites as main remanence carriers, and their domain structure is characterised by a mixture of single-domain and multi-domain grains. Characteristic paleomagnetic directions are retrieved from 28 out of 29 sites (235 standard paleomagnetic cores). 17 sites show normal polarity, 10 sites show reverse polarity and one site shows an oblique direction, with negative inclination, separated 79° of the mean normal directions. The reversal test is positive at the 95% confidence level which ensures that the secondary remanent magnetizations were successfully removed and the sampling adequately averaged the palaeosecular variation. The paleosecular variation parameters values obtained in this study correlate with those determined for the Cretaceous Normal Superchron, between 125 to 84 Ma. The new paleomagnetic pole position (222.0° E, 88.1° S, N = 24, K = 35.68, A95 = 5.0°) agrees well (within uncertainties) with the reference poles determined from Besse and Courtillot (2002), and disagree with those reported in previous studies. The new results should be considered for estimating the Cretaceous paleomagnetic poles for stable South America.Fil: Cervantes Solano, Miguel. Universidad Nacional Autónoma de México; MéxicoFil: Goguitchaichvili, Avto. Universidad Nacional Autónoma de México; MéxicoFil: Mena, Mabel. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geociencias Basicas, Aplicadas y Ambientales de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geociencias Basicas, Aplicadas y Ambientales de Buenos Aires; ArgentinaFil: Alva Valdivia, Luis. Instituto Potosino de Investigación Científica y Tecnológica; MéxicoFil: Morales Contreras, Juan. Universidad Nacional Autónoma de México; MéxicoFil: Cejudo Ruiz, Rubén. Universidad Nacional Autónoma de México; MéxicoFil: López Loera, Héctor. Instituto Potosino de Investigación Científica y Tecnológica; MéxicoFil: Soler, Ana María. Instituto Potosino de Investigación Científica y Tecnológica; MéxicoFil: Urrutia Fucugauchi, Jaime. Universidad Nacional Autónoma de México; MéxicoUniversidad Nacional Autónoma de México. Instituto de Geofísica2015-05info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/20776Cervantes Solano, Miguel; Goguitchaichvili, Avto; Mena, Mabel; Alva Valdivia, Luis; Morales Contreras, Juan; et al.; Paleomagnetic Pole Positions and Geomagnetic Secular Variation from the Cretaceous Ponta Grossa Dike Swarm (Brazil); Universidad Nacional Autónoma de México. Instituto de Geofísica; Geofísica Internacional; 54; 2; 5-2015; 167-1780016-7169CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/10.1016/j.gi.2015.04.012info:eu-repo/semantics/altIdentifier/url/http://www.sciencedirect.com/science/article/pii/S0016716915000136info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-nd/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-03T09:57:28Zoai:ri.conicet.gov.ar:11336/20776instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-09-03 09:57:28.475CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
dc.title.none.fl_str_mv |
Paleomagnetic Pole Positions and Geomagnetic Secular Variation from the Cretaceous Ponta Grossa Dike Swarm (Brazil) |
title |
Paleomagnetic Pole Positions and Geomagnetic Secular Variation from the Cretaceous Ponta Grossa Dike Swarm (Brazil) |
spellingShingle |
Paleomagnetic Pole Positions and Geomagnetic Secular Variation from the Cretaceous Ponta Grossa Dike Swarm (Brazil) Cervantes Solano, Miguel Ponta Grossa Dike Swarm South America Paleomagnetism Cretaceous |
title_short |
Paleomagnetic Pole Positions and Geomagnetic Secular Variation from the Cretaceous Ponta Grossa Dike Swarm (Brazil) |
title_full |
Paleomagnetic Pole Positions and Geomagnetic Secular Variation from the Cretaceous Ponta Grossa Dike Swarm (Brazil) |
title_fullStr |
Paleomagnetic Pole Positions and Geomagnetic Secular Variation from the Cretaceous Ponta Grossa Dike Swarm (Brazil) |
title_full_unstemmed |
Paleomagnetic Pole Positions and Geomagnetic Secular Variation from the Cretaceous Ponta Grossa Dike Swarm (Brazil) |
title_sort |
Paleomagnetic Pole Positions and Geomagnetic Secular Variation from the Cretaceous Ponta Grossa Dike Swarm (Brazil) |
dc.creator.none.fl_str_mv |
Cervantes Solano, Miguel Goguitchaichvili, Avto Mena, Mabel Alva Valdivia, Luis Morales Contreras, Juan Cejudo Ruiz, Rubén López Loera, Héctor Soler, Ana María Urrutia Fucugauchi, Jaime |
author |
Cervantes Solano, Miguel |
author_facet |
Cervantes Solano, Miguel Goguitchaichvili, Avto Mena, Mabel Alva Valdivia, Luis Morales Contreras, Juan Cejudo Ruiz, Rubén López Loera, Héctor Soler, Ana María Urrutia Fucugauchi, Jaime |
author_role |
author |
author2 |
Goguitchaichvili, Avto Mena, Mabel Alva Valdivia, Luis Morales Contreras, Juan Cejudo Ruiz, Rubén López Loera, Héctor Soler, Ana María Urrutia Fucugauchi, Jaime |
author2_role |
author author author author author author author author |
dc.subject.none.fl_str_mv |
Ponta Grossa Dike Swarm South America Paleomagnetism Cretaceous |
topic |
Ponta Grossa Dike Swarm South America Paleomagnetism Cretaceous |
purl_subject.fl_str_mv |
https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
dc.description.none.fl_txt_mv |
A detailed paleomagnetic and rock magnetic investigation has been carried out on the Early Cretaceous Ponta Grossa dike swarm in southern Brazil. This formation seems an excellent target for paleomagnetic study. The dikes are widely distributed over a large area, easy to access, and they record faithfully the geomagnetic field at the time of the eruption. Most of them are fresh and have been dated by K-Ar and Ar-Ar. Thermomagnetic experiments (low-field versus temperature curves) suggest low-Ti titanomagnetites as main remanence carriers, and their domain structure is characterised by a mixture of single-domain and multi-domain grains. Characteristic paleomagnetic directions are retrieved from 28 out of 29 sites (235 standard paleomagnetic cores). 17 sites show normal polarity, 10 sites show reverse polarity and one site shows an oblique direction, with negative inclination, separated 79° of the mean normal directions. The reversal test is positive at the 95% confidence level which ensures that the secondary remanent magnetizations were successfully removed and the sampling adequately averaged the palaeosecular variation. The paleosecular variation parameters values obtained in this study correlate with those determined for the Cretaceous Normal Superchron, between 125 to 84 Ma. The new paleomagnetic pole position (222.0° E, 88.1° S, N = 24, K = 35.68, A95 = 5.0°) agrees well (within uncertainties) with the reference poles determined from Besse and Courtillot (2002), and disagree with those reported in previous studies. The new results should be considered for estimating the Cretaceous paleomagnetic poles for stable South America. Fil: Cervantes Solano, Miguel. Universidad Nacional Autónoma de México; México Fil: Goguitchaichvili, Avto. Universidad Nacional Autónoma de México; México Fil: Mena, Mabel. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geociencias Basicas, Aplicadas y Ambientales de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geociencias Basicas, Aplicadas y Ambientales de Buenos Aires; Argentina Fil: Alva Valdivia, Luis. Instituto Potosino de Investigación Científica y Tecnológica; México Fil: Morales Contreras, Juan. Universidad Nacional Autónoma de México; México Fil: Cejudo Ruiz, Rubén. Universidad Nacional Autónoma de México; México Fil: López Loera, Héctor. Instituto Potosino de Investigación Científica y Tecnológica; México Fil: Soler, Ana María. Instituto Potosino de Investigación Científica y Tecnológica; México Fil: Urrutia Fucugauchi, Jaime. Universidad Nacional Autónoma de México; México |
description |
A detailed paleomagnetic and rock magnetic investigation has been carried out on the Early Cretaceous Ponta Grossa dike swarm in southern Brazil. This formation seems an excellent target for paleomagnetic study. The dikes are widely distributed over a large area, easy to access, and they record faithfully the geomagnetic field at the time of the eruption. Most of them are fresh and have been dated by K-Ar and Ar-Ar. Thermomagnetic experiments (low-field versus temperature curves) suggest low-Ti titanomagnetites as main remanence carriers, and their domain structure is characterised by a mixture of single-domain and multi-domain grains. Characteristic paleomagnetic directions are retrieved from 28 out of 29 sites (235 standard paleomagnetic cores). 17 sites show normal polarity, 10 sites show reverse polarity and one site shows an oblique direction, with negative inclination, separated 79° of the mean normal directions. The reversal test is positive at the 95% confidence level which ensures that the secondary remanent magnetizations were successfully removed and the sampling adequately averaged the palaeosecular variation. The paleosecular variation parameters values obtained in this study correlate with those determined for the Cretaceous Normal Superchron, between 125 to 84 Ma. The new paleomagnetic pole position (222.0° E, 88.1° S, N = 24, K = 35.68, A95 = 5.0°) agrees well (within uncertainties) with the reference poles determined from Besse and Courtillot (2002), and disagree with those reported in previous studies. The new results should be considered for estimating the Cretaceous paleomagnetic poles for stable South America. |
publishDate |
2015 |
dc.date.none.fl_str_mv |
2015-05 |
dc.type.none.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion http://purl.org/coar/resource_type/c_6501 info:ar-repo/semantics/articulo |
format |
article |
status_str |
publishedVersion |
dc.identifier.none.fl_str_mv |
http://hdl.handle.net/11336/20776 Cervantes Solano, Miguel; Goguitchaichvili, Avto; Mena, Mabel; Alva Valdivia, Luis; Morales Contreras, Juan; et al.; Paleomagnetic Pole Positions and Geomagnetic Secular Variation from the Cretaceous Ponta Grossa Dike Swarm (Brazil); Universidad Nacional Autónoma de México. Instituto de Geofísica; Geofísica Internacional; 54; 2; 5-2015; 167-178 0016-7169 CONICET Digital CONICET |
url |
http://hdl.handle.net/11336/20776 |
identifier_str_mv |
Cervantes Solano, Miguel; Goguitchaichvili, Avto; Mena, Mabel; Alva Valdivia, Luis; Morales Contreras, Juan; et al.; Paleomagnetic Pole Positions and Geomagnetic Secular Variation from the Cretaceous Ponta Grossa Dike Swarm (Brazil); Universidad Nacional Autónoma de México. Instituto de Geofísica; Geofísica Internacional; 54; 2; 5-2015; 167-178 0016-7169 CONICET Digital CONICET |
dc.language.none.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
info:eu-repo/semantics/altIdentifier/doi/10.1016/j.gi.2015.04.012 info:eu-repo/semantics/altIdentifier/url/http://www.sciencedirect.com/science/article/pii/S0016716915000136 |
dc.rights.none.fl_str_mv |
info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-nd/2.5/ar/ |
eu_rights_str_mv |
openAccess |
rights_invalid_str_mv |
https://creativecommons.org/licenses/by-nc-nd/2.5/ar/ |
dc.format.none.fl_str_mv |
application/pdf application/pdf |
dc.publisher.none.fl_str_mv |
Universidad Nacional Autónoma de México. Instituto de Geofísica |
publisher.none.fl_str_mv |
Universidad Nacional Autónoma de México. Instituto de Geofísica |
dc.source.none.fl_str_mv |
reponame:CONICET Digital (CONICET) instname:Consejo Nacional de Investigaciones Científicas y Técnicas |
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CONICET Digital (CONICET) |
collection |
CONICET Digital (CONICET) |
instname_str |
Consejo Nacional de Investigaciones Científicas y Técnicas |
repository.name.fl_str_mv |
CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas |
repository.mail.fl_str_mv |
dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar |
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1842269463599120384 |
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13.13397 |