Etudes sur le comportement du champ magnétique terrestre durant les périodes de polarité stable

Autor: Bouligand, Claire

Le comportement du champ magnétique de la Terre, à l'échelle d'un intervalle de polarité, peut être représenté à l'aide de modèles statistiques de type "Giant Gaussian Process" (GGP) permettant de décrire la valeur du champ moyen et la vari

Externí odkaz: http://tel.archives-ouvertes.fr/tel-00676769
http://tel.archives-ouvertes.fr/docs/00/67/67/69/PDF/these_Bouligand.pdf

Sub-surface structure of La Soufrière of Guadeloupe lava dome deduced from a ground-based magnetic survey

Autor: Bouligand, Claire, Coutant, Olivier, Glen, Jonathan M.G.

Publikováno v: In Journal of Volcanology and Geothermal Research 15 July 2016 321:171-181

A 9 million-year-long astrochronological record of the early- middle Eocene corroborated by seafloor spreading rates

Autor: Francescone, Federica, Lauretano, Vittoria, Bouligand, Claire, Moretti, Matteo, Sabatino, Nadia, Schrader, Cindy, Catanzariti, Rita, Hilgen, Frits, Lanci, Luca, Turtù, Antonio, Sprovieri, Mario, Lourens, Lucas, Galeotti, Simone, Stratigraphy & paleontology, Stratigraphy and paleontology

Publikováno v: Bulletin of the Geological Society of America, 131(3-4), 499-520. Geological Society of America
Francescone, F, Lauretano, V, Bouligand, C, Moretti, M, Sabatino, N, Schrader, C, Catanzariti, R, Hilgen, F, Lanci, L, Turtù, A, Sprovieri, M, Lourens, L & Galeotti, S 2018, ' A 9 million-year-long astrochronological record of the early-middle Eocene corroborated by seafloor spreading rates ', Bulletin of the Geological Society of America, vol. 131, no. 3-4, pp. 499-520 . https://doi.org/10.1130/B32050.1
Geological Society of America bulletin 131 (2019): 499–520. doi:10.1130/B32050.1
info:cnr-pdr/source/autori:Francescone F.[1], Lauretano V.[2], Bouligand C.[3], Moretti M.[1], Sabatino N.[4], Schrader C.[5], Catanzariti R.[6], Hilgen F.[5], Lanci L.[1], Turtù A.[7], Sprovieri M.[4], Lourens L.[5], Galeotti S.[1]/titolo:A 9 million-year-long astrochronological record of the early-middle Eocene corroborated by seafloor spreading rates/doi:10.1130%2FB32050.1/rivista:Geological Society of America bulletin/anno:2019/pagina_da:499/pagina_a:520/intervallo_pagine:499–520/volume:131
Geological Society of America Bulletin, 131(3-4), 499. Geological Society of America

The early-middle Eocene (ca. 56-41 Ma) is recorded in the pelagic Scaglia Rossa and Variegata Formations of the Umbria-Marche Basin (central Italy). Geochemical and magnetostratigraphic alignment between the Bottaccione section (Gubbio, central Italy

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::62463d923dc25ee173edd06fa9babef2
https://hdl.handle.net/1871.1/d53958da-9c95-4c97-a299-c2039953ef60

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Heat and Mass Transport in a Vapor‐Dominated Hydrothermal Area in Yellowstone National Park, USA: Inferences From Magnetic, Electrical, Electromagnetic, Subsurface Temperature, and Diffuse CO2 Flux Measurements.

Autor: Bouligand, Claire, Hurwitz, Shaul, Vandemeulebrouck, Jean, Byrdina, Svetlana, Kass, Mason Andrew, Lewicki, Jennifer Lynn

Publikováno v: Journal of Geophysical Research. Solid Earth; Jan2019, Vol. 124 Issue 1, p291-309, 19p