Vortex Magnetic Domain State Behavior in the Day Plot
- Autores
- Williams, Wyn; Moreno Ortega, Roberto; Muxworthy, Adrian R.; Paterson, Greig A.; Nagy, Lesleis; Tauxe, Lisa; Donardelli Bellon, Ualisson; Cowan, Alison A.; Ferreira, Idenildo
- Año de publicación
- 2024
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- The ability of rocks to hold a reliable record of the ancient geomagnetic field depends on the structure and stability of magnetic domain‐states contained within constituent particles. In paleomagnetic studies, the Day plot is an easily constructed graph of magnetic hysteresis parameters that is frequently used to estimate the likely magnetic recording stability of samples. Often samples plot in the region of the Day plot attributed to so‐called pseudo‐single‐domain particles with little understanding of the implications for domain‐ states or recording fidelity. Here we use micromagnetic models to explore the hysteresis parameters of magnetite particles with idealized prolate and oblate truncated‐octahedral geometries containing single domain (SD), single‐vortex and occasionally multi‐vortex states. We show that these domain states exhibit a well‐ defined trend in the Day plot that extends from the SD region well into the multi‐domain region, all of which are likely to be stable remanence carriers. We suggest that although the interpretation of the Day plot and its variants might be subject to ambiguities, if the magnetic mineralogy is known, it can still provide some useful insights about paleomagnetic specimens' dominant domain state, average particle sizes and, consequently, their paleomagnetic stability.
Fil: Williams, Wyn. University of Edinburgh; Reino Unido
Fil: Moreno Ortega, Roberto. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Córdoba. Instituto de Física Enrique Gaviola. Universidad Nacional de Córdoba. Instituto de Física Enrique Gaviola; Argentina
Fil: Muxworthy, Adrian R.. Imperial College London; Reino Unido
Fil: Paterson, Greig A.. University of Liverpool; Reino Unido
Fil: Nagy, Lesleis. University of Liverpool; Reino Unido
Fil: Tauxe, Lisa. University of California at San Diego. Scripps Institution of Oceanography; Estados Unidos
Fil: Donardelli Bellon, Ualisson. Universidade do Sao Paulo. Instituto de Astronomia, Geofísica e Ciências Atmosféricas; Brasil
Fil: Cowan, Alison A.. Imperial College London; Reino Unido
Fil: Ferreira, Idenildo. University of Edinburgh; Reino Unido - Materia
- Day Plot
- Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- https://creativecommons.org/licenses/by/2.5/ar/
- Repositorio
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/268666
Ver los metadatos del registro completo
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Vortex Magnetic Domain State Behavior in the Day PlotWilliams, WynMoreno Ortega, RobertoMuxworthy, Adrian R.Paterson, Greig A.Nagy, LesleisTauxe, LisaDonardelli Bellon, UalissonCowan, Alison A.Ferreira, IdenildoDay Plothttps://purl.org/becyt/ford/1.7https://purl.org/becyt/ford/1The ability of rocks to hold a reliable record of the ancient geomagnetic field depends on the structure and stability of magnetic domain‐states contained within constituent particles. In paleomagnetic studies, the Day plot is an easily constructed graph of magnetic hysteresis parameters that is frequently used to estimate the likely magnetic recording stability of samples. Often samples plot in the region of the Day plot attributed to so‐called pseudo‐single‐domain particles with little understanding of the implications for domain‐ states or recording fidelity. Here we use micromagnetic models to explore the hysteresis parameters of magnetite particles with idealized prolate and oblate truncated‐octahedral geometries containing single domain (SD), single‐vortex and occasionally multi‐vortex states. We show that these domain states exhibit a well‐ defined trend in the Day plot that extends from the SD region well into the multi‐domain region, all of which are likely to be stable remanence carriers. We suggest that although the interpretation of the Day plot and its variants might be subject to ambiguities, if the magnetic mineralogy is known, it can still provide some useful insights about paleomagnetic specimens' dominant domain state, average particle sizes and, consequently, their paleomagnetic stability.Fil: Williams, Wyn. University of Edinburgh; Reino UnidoFil: Moreno Ortega, Roberto. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Córdoba. Instituto de Física Enrique Gaviola. Universidad Nacional de Córdoba. Instituto de Física Enrique Gaviola; ArgentinaFil: Muxworthy, Adrian R.. Imperial College London; Reino UnidoFil: Paterson, Greig A.. University of Liverpool; Reino UnidoFil: Nagy, Lesleis. University of Liverpool; Reino UnidoFil: Tauxe, Lisa. University of California at San Diego. Scripps Institution of Oceanography; Estados UnidosFil: Donardelli Bellon, Ualisson. Universidade do Sao Paulo. Instituto de Astronomia, Geofísica e Ciências Atmosféricas; BrasilFil: Cowan, Alison A.. Imperial College London; Reino UnidoFil: Ferreira, Idenildo. University of Edinburgh; Reino UnidoAmerican Geophysical Union2024-08info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/268666Williams, Wyn; Moreno Ortega, Roberto; Muxworthy, Adrian R.; Paterson, Greig A.; Nagy, Lesleis; et al.; Vortex Magnetic Domain State Behavior in the Day Plot; American Geophysical Union; Geochemistry Geophysics Geosystems; 25; 8; 8-2024; 1-171525-2027CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2024GC011462info:eu-repo/semantics/altIdentifier/doi/10.1029/2024GC011462info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-03T10:08:00Zoai:ri.conicet.gov.ar:11336/268666instacron: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 10:08:00.263CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
dc.title.none.fl_str_mv |
Vortex Magnetic Domain State Behavior in the Day Plot |
title |
Vortex Magnetic Domain State Behavior in the Day Plot |
spellingShingle |
Vortex Magnetic Domain State Behavior in the Day Plot Williams, Wyn Day Plot |
title_short |
Vortex Magnetic Domain State Behavior in the Day Plot |
title_full |
Vortex Magnetic Domain State Behavior in the Day Plot |
title_fullStr |
Vortex Magnetic Domain State Behavior in the Day Plot |
title_full_unstemmed |
Vortex Magnetic Domain State Behavior in the Day Plot |
title_sort |
Vortex Magnetic Domain State Behavior in the Day Plot |
dc.creator.none.fl_str_mv |
Williams, Wyn Moreno Ortega, Roberto Muxworthy, Adrian R. Paterson, Greig A. Nagy, Lesleis Tauxe, Lisa Donardelli Bellon, Ualisson Cowan, Alison A. Ferreira, Idenildo |
author |
Williams, Wyn |
author_facet |
Williams, Wyn Moreno Ortega, Roberto Muxworthy, Adrian R. Paterson, Greig A. Nagy, Lesleis Tauxe, Lisa Donardelli Bellon, Ualisson Cowan, Alison A. Ferreira, Idenildo |
author_role |
author |
author2 |
Moreno Ortega, Roberto Muxworthy, Adrian R. Paterson, Greig A. Nagy, Lesleis Tauxe, Lisa Donardelli Bellon, Ualisson Cowan, Alison A. Ferreira, Idenildo |
author2_role |
author author author author author author author author |
dc.subject.none.fl_str_mv |
Day Plot |
topic |
Day Plot |
purl_subject.fl_str_mv |
https://purl.org/becyt/ford/1.7 https://purl.org/becyt/ford/1 |
dc.description.none.fl_txt_mv |
The ability of rocks to hold a reliable record of the ancient geomagnetic field depends on the structure and stability of magnetic domain‐states contained within constituent particles. In paleomagnetic studies, the Day plot is an easily constructed graph of magnetic hysteresis parameters that is frequently used to estimate the likely magnetic recording stability of samples. Often samples plot in the region of the Day plot attributed to so‐called pseudo‐single‐domain particles with little understanding of the implications for domain‐ states or recording fidelity. Here we use micromagnetic models to explore the hysteresis parameters of magnetite particles with idealized prolate and oblate truncated‐octahedral geometries containing single domain (SD), single‐vortex and occasionally multi‐vortex states. We show that these domain states exhibit a well‐ defined trend in the Day plot that extends from the SD region well into the multi‐domain region, all of which are likely to be stable remanence carriers. We suggest that although the interpretation of the Day plot and its variants might be subject to ambiguities, if the magnetic mineralogy is known, it can still provide some useful insights about paleomagnetic specimens' dominant domain state, average particle sizes and, consequently, their paleomagnetic stability. Fil: Williams, Wyn. University of Edinburgh; Reino Unido Fil: Moreno Ortega, Roberto. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Córdoba. Instituto de Física Enrique Gaviola. Universidad Nacional de Córdoba. Instituto de Física Enrique Gaviola; Argentina Fil: Muxworthy, Adrian R.. Imperial College London; Reino Unido Fil: Paterson, Greig A.. University of Liverpool; Reino Unido Fil: Nagy, Lesleis. University of Liverpool; Reino Unido Fil: Tauxe, Lisa. University of California at San Diego. Scripps Institution of Oceanography; Estados Unidos Fil: Donardelli Bellon, Ualisson. Universidade do Sao Paulo. Instituto de Astronomia, Geofísica e Ciências Atmosféricas; Brasil Fil: Cowan, Alison A.. Imperial College London; Reino Unido Fil: Ferreira, Idenildo. University of Edinburgh; Reino Unido |
description |
The ability of rocks to hold a reliable record of the ancient geomagnetic field depends on the structure and stability of magnetic domain‐states contained within constituent particles. In paleomagnetic studies, the Day plot is an easily constructed graph of magnetic hysteresis parameters that is frequently used to estimate the likely magnetic recording stability of samples. Often samples plot in the region of the Day plot attributed to so‐called pseudo‐single‐domain particles with little understanding of the implications for domain‐ states or recording fidelity. Here we use micromagnetic models to explore the hysteresis parameters of magnetite particles with idealized prolate and oblate truncated‐octahedral geometries containing single domain (SD), single‐vortex and occasionally multi‐vortex states. We show that these domain states exhibit a well‐ defined trend in the Day plot that extends from the SD region well into the multi‐domain region, all of which are likely to be stable remanence carriers. We suggest that although the interpretation of the Day plot and its variants might be subject to ambiguities, if the magnetic mineralogy is known, it can still provide some useful insights about paleomagnetic specimens' dominant domain state, average particle sizes and, consequently, their paleomagnetic stability. |
publishDate |
2024 |
dc.date.none.fl_str_mv |
2024-08 |
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/11336/268666 Williams, Wyn; Moreno Ortega, Roberto; Muxworthy, Adrian R.; Paterson, Greig A.; Nagy, Lesleis; et al.; Vortex Magnetic Domain State Behavior in the Day Plot; American Geophysical Union; Geochemistry Geophysics Geosystems; 25; 8; 8-2024; 1-17 1525-2027 CONICET Digital CONICET |
url |
http://hdl.handle.net/11336/268666 |
identifier_str_mv |
Williams, Wyn; Moreno Ortega, Roberto; Muxworthy, Adrian R.; Paterson, Greig A.; Nagy, Lesleis; et al.; Vortex Magnetic Domain State Behavior in the Day Plot; American Geophysical Union; Geochemistry Geophysics Geosystems; 25; 8; 8-2024; 1-17 1525-2027 CONICET Digital CONICET |
dc.language.none.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
info:eu-repo/semantics/altIdentifier/url/https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2024GC011462 info:eu-repo/semantics/altIdentifier/doi/10.1029/2024GC011462 |
dc.rights.none.fl_str_mv |
info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by/2.5/ar/ |
eu_rights_str_mv |
openAccess |
rights_invalid_str_mv |
https://creativecommons.org/licenses/by/2.5/ar/ |
dc.format.none.fl_str_mv |
application/pdf application/pdf |
dc.publisher.none.fl_str_mv |
American Geophysical Union |
publisher.none.fl_str_mv |
American Geophysical Union |
dc.source.none.fl_str_mv |
reponame:CONICET Digital (CONICET) instname:Consejo Nacional de Investigaciones Científicas y Técnicas |
reponame_str |
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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1842270026824941568 |
score |
13.13397 |