Clastic Polygonal Networks Around Lyot Crater, Mars: Possible Formation Mechanisms from Morphometric Analysis L.M
Clastic polygonal networks around Lyot crater, Mars: Possible formation mechanisms from morphometric analysis L.M. Brooker, M.R. Balme, S.J. Conway, A. Hagermann, A. Barrett, G.S. Collins, R.J. Soare To cite this version: L.M. Brooker, M.R. Balme, S.J. Conway, A. Hagermann, A. Barrett, et al.. Clastic polygonal net- works around Lyot crater, Mars: Possible formation mechanisms from morphometric analysis. Icarus, Elsevier, 2018, 302, pp.386-406. 10.1016/j.icarus.2017.11.022. hal-02269969 HAL Id: hal-02269969 https://hal.archives-ouvertes.fr/hal-02269969 Submitted on 23 Aug 2019 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Icarus 302 (2018) 386–406 Contents lists available at ScienceDirect Icarus journal homepage: www.elsevier.com/locate/icarus Clastic polygonal networks around Lyot crater, Mars: Possible formation mechanisms from morphometric analysis ∗ L.M. Brooker a, , M.R. Balme a, S.J. Conway b, A. Hagermann a, A.M. Barrett a, G.S. Collins c, R.J. Soare d a Department of Physical Sciences, Open University, Walton Hall, Milton Keynes MK7 6AA, UK b CNRS Laboratoire de Planétologie et Géodynamique de Nantes, Université de Nantes, 2 rue de la Houssiniére, 44322 Nantes, France c Department of Earth Science and Engineering, Imperial College, Kensington, London SW7 2BP, UK d Department of Geography, Dawson College, Montreal H3Z 1A4, Canada a r t i c l e i n f o a b s t r a c t Article history: Polygonal networks of patterned ground are a common feature in cold-climate environments.
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