Initial results of the Netlander imaging ground-penetrating radaroperated on the Antarctic Ice Shelf

The objective of the Netlander mission was to land 4 small geophysical stations on the surface of Mars to study the deep interior, subsurface, surface and atmosphere of the planet. Included in the payload was a ground penetrating radar (GPR) designed to retrieve not only the distance but also the di...

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Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: Berthelier, Jean-Jacques, Bonaimé, S., Ciarletti, Valérie, Clairquin, R., Dolon, F., Le Gall, Alice, Nevejans, D., Ney, Richard, Reineix, Alain
Other Authors: Centre d'étude des environnements terrestre et planétaires (CETP), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Institut de Physique du Globe de Paris (IPGP), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-Université de La Réunion (UR)-Institut de Physique du Globe de Paris (IPG Paris)-Centre National de la Recherche Scientifique (CNRS), Belgian Institute for Space Aeronomy / Institut d'Aéronomie Spatiale de Belgique (BIRA-IASB), OSA, XLIM (XLIM), Université de Limoges (UNILIM)-Centre National de la Recherche Scientifique (CNRS)-Université de Limoges (UNILIM)-Centre National de la Recherche Scientifique (CNRS), CNES (grants 793/CNES/99/7947 and 737/CNES/00/8261)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2006
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Online Access:https://hal.science/hal-00159138
https://hal.science/hal-00159138/document
https://hal.science/hal-00159138/file/Berthelier_et_al-2005-Geophysical_Research_Letters.pdf
https://doi.org/10.1029/2005GL024203
Description
Summary:The objective of the Netlander mission was to land 4 small geophysical stations on the surface of Mars to study the deep interior, subsurface, surface and atmosphere of the planet. Included in the payload was a ground penetrating radar (GPR) designed to retrieve not only the distance but also the direction of the reflectors, thus providing a simplified 3D imaging of the subsurface. In this paper we report initial results obtained during the RANETA campaign on the Antarctic ice shelf. Data from two soundings of the ice-bed rock interface are analyzed, demonstrating the capability of the radar to disentangle echoes from different reflecting facets of the bed rock.