Molards as an analogue for ejecta-ice interactions on Mars

International audience The 125-km-diameter Hale impact crater is located in the southern hemisphere of Mars and has been dated to 1 Ga (Early to Middle Amazonian; Jones et al., 2011). It is thought to have penetrated the martian cryosphere, because it hosts landforms indicating volatile mobilisation...

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Bibliographic Details
Main Authors: Morino, Costanza, Conway, Susan J., Peignaux, Coralie, Lucas, Antoine, Svennevig, Kristian, Butcher, Frances, Roberti, Gioachino, Philippe, Meven, Collins-May, Jake
Other Authors: Environnements, Dynamiques et Territoires de Montagne (EDYTEM), Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS), Laboratoire de Planétologie et Géodynamique UMR 6112 (LPG), Université d'Angers (UA)-Université de Nantes - UFR des Sciences et des Techniques (UN UFR ST), Université de Nantes (UN)-Université de Nantes (UN)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Institut de Physique du Globe de Paris (IPGP (UMR_7154)), Institut national des sciences de l'Univers (INSU - CNRS)-Université de La Réunion (UR)-Institut de Physique du Globe de Paris (IPG Paris)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité), Geological Survey of Denmark and Greenland (GEUS), University of Sheffield Sheffield, Minerva Intelligence Inc., The School of Geography, Politics and Sociology; Newcastle University, ANR-19-CE01-0010,Permolards,Les molards, marqueurs de l'évolution de la dégradation du pergélisol de montagne(2019)
Format: Conference Object
Language:English
Published: HAL CCSD 2021
Subjects:
[SDU.STU.PL]Sciences of the Universe [physics]/Earth Sciences/Planetology
[SDU.STU.GM]Sciences of the Universe [physics]/Earth Sciences/Geomorphology
Canada
Greenland
Hale
Paatuut
Online Access:https://hal.science/hal-03280950
https://hal.science/hal-03280950v2/document
https://hal.science/hal-03280950v2/file/EGU21-9628-print.pdf
https://doi.org/10.5194/egusphere-egu21-9628

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