Zobrazeno 1 - 10
of 15
pro vyhledávání: '"Alberto Molina‐Cardín"'
Autor:
Alicia González-López, María Luisa Osete, Saioa A. Campuzano, Alberto Molina-Cardín, Pablo Rivera, Francisco Javier Pavón-Carrasco
Publikováno v:
Geosciences, Vol 11, Iss 11, p 438 (2021)
The eccentric dipole (ED) is the next approach of the geomagnetic field after the generally used geocentric dipole. Here, we analyzed the evolution of the ED during extreme events, such as the Matuyama-Brunhes polarity transition (~780 ka), the Lasch
Externí odkaz:
https://doaj.org/article/ef9981af89134397881cadcdae54a0a3
Autor:
Alicia González-López, Maria Luisa Osete, Saioa A. Campuzano, Pablo Rivera-Pérez, Alberto Molina-Cardín, F. Javier Pavón-Carrasco
Eccentric dipole can be considered the next approximation of the geomagnetic field after thegenerally used geocentric dipole. Considering that during reversals, excursions and importantanomalies the non-dipole contributions are relevant, we study the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::71fabcd4bc65a8caa9e7e813f17b757a
https://doi.org/10.5194/egusphere-egu22-8344
https://doi.org/10.5194/egusphere-egu22-8344
Autor:
José Carlos Sastre Blanco, David Sánchez Nicolás, Israel Espí Pérez, Alberto Molina Cardín, Saioa A. Campuzano, Alicia Palencia Ortas, Gregg McIntosh, María Luisa Osete
Publikováno v:
Complutum; Vol. 33 Núm. 1 (2022); 159-176
Complutum; Vol. 33 No. 1 (2022); 159-176
Revistas Científicas Complutenses
Universidad Complutense de Madrid (UCM)
Complutum; Vol. 33 No. 1 (2022); 159-176
Revistas Científicas Complutenses
Universidad Complutense de Madrid (UCM)
The archaeological excavation undertaken at Quinta de Crestelos (Merinhos, Mogadouro, Portugal), revealed a large occupation site dated between Late Iron Age and Early Roman periods. On the ridge top a small fortified site with elaborated defensive s
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8b626ea12ce6a5c4c705fbfbe29d4e18
https://revistas.ucm.es/index.php/CMPL/article/view/80890
https://revistas.ucm.es/index.php/CMPL/article/view/80890
Autor:
Alberto Molina‐Cardín, Saioa A. Campuzano, Francisco Javier Pavón-Carrasco, Pablo Rivera, Alicia González-López, María Luisa Osete
Publikováno v:
Geosciences
Volume 11
Issue 11
E-Prints Complutense. Archivo Institucional de la UCM
instname
Geosciences, Vol 11, Iss 438, p 438 (2021)
Volume 11
Issue 11
E-Prints Complutense. Archivo Institucional de la UCM
instname
Geosciences, Vol 11, Iss 438, p 438 (2021)
The eccentric dipole (ED) is the next approach of the geomagnetic field after the generally used geocentric dipole. Here, we analyzed the evolution of the ED during extreme events, such as the Matuyama-Brunhes polarity transition (~780 ka), the Lasch
Autor:
Fátima Martín-Hernández, Annick Chauvin, Pierrick Roperch, María Luisa Osete, A. Palencia-Ortas, Alberto Molina‐Cardín, Miriam Gómez-Paccard
Publikováno v:
Physics of the Earth and Planetary Interiors
Physics of the Earth and Planetary Interiors, 2021, 318, pp.106762. ⟨10.1016/j.pepi.2021.106762⟩
Physics of the Earth and Planetary Interiors, Elsevier, 2021, 318, pp.106762. ⟨10.1016/j.pepi.2021.106762⟩
Physics of the Earth and Planetary Interiors, 2021, 318, pp.106762. ⟨10.1016/j.pepi.2021.106762⟩
Physics of the Earth and Planetary Interiors, Elsevier, 2021, 318, pp.106762. ⟨10.1016/j.pepi.2021.106762⟩
International audience; In directional archaeomagnetic studies, it is rarely analysed whether the combustion structures display anisotropy of their thermoremanent magnetization (ATRM). It has been observed that, in specific cases like thin baked clay
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f8f3271c4abd5734357b261a65314cb8
https://insu.hal.science/insu-03331680
https://insu.hal.science/insu-03331680
Autor:
Angelo De Santis, Alberto Molina Cardín, Saioa A. Campuzano, Martina Orlando, F. Javier Pavon-Carrasco
The Shannon Information or Information Content is a statistical measure of a system characterising its properties of organisation (maximum value) or disorder (minimum value). Once it is introduced the scalar potential of the geomagnetic field in term
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::694db09da7e6115509df4ab10fd3e443
https://doi.org/10.5194/egusphere-egu21-5305
https://doi.org/10.5194/egusphere-egu21-5305
Autor:
Alicia González-López, Saioa A. Campuzano, Pablo Rivera, Alberto Molina-Cardín, F. Javier Pavón-Carrasco, M. Luisa Osete
The geomagnetic field is commonly approximated to a geocentric tilted dipole. However, a next step in the approach of the geomagnetic field is the eccentric dipole which takes the first and second terms of the spherical harmonic representation of the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e52f498c310bf281a69a7e440981ecac
https://doi.org/10.5194/egusphere-egu21-4237
https://doi.org/10.5194/egusphere-egu21-4237
Autor:
Alberto Molina‐Cardín, M. Luisa Osete, M. Rivero-Montero, Saioa A. Campuzano, Miriam Gómez-Paccard, F. Javier Pavón-Carrasco
Publikováno v:
E-Prints Complutense. Archivo Institucional de la UCM
Instituto de Salud Carlos III (ISCIII)
Instituto de Salud Carlos III (ISCIII)
Since the publication of the European archaeomagnetic field model SCHA.DIF.3k in 2009, the number of paleomagnetic data derived from archaeological materials such as baked clays and volcanic rocks coming from Europe has increased by about 90% for dir
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::cd6efab81a1c251cfdea23d2eb3aad27
https://eprints.ucm.es/id/eprint/65864/
https://eprints.ucm.es/id/eprint/65864/
Autor:
Alicia González-López, Angelo De Santis, Francisco Javier Pavón-Carrasco, María Luisa Osete, Saioa A. Campuzano, Alberto Molina‐Cardín
Temporal changes in the main geomagnetic field, the so-called secular variation, can range from decades to millennia without showing any clear periodicity. A better knowledge of the secular variation behaviour is important to determine the mechanisms
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a6b99c12a801b2986134c121733f0828
https://doi.org/10.5194/egusphere-egu2020-449
https://doi.org/10.5194/egusphere-egu2020-449
The magnetic field of the Earth is generated in its core by the process called the geodynamo, which involves convection in the fluid and electrical conducting outer core. The evolution of this complex process is simulated by magnetohydrodynamic model
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::71c9eacfc8e268ff507175343d8db49a
https://doi.org/10.5194/egusphere-egu2020-19012
https://doi.org/10.5194/egusphere-egu2020-19012