Largest recent impact craters on Mars: Orbital imaging and surface seismic co-investigation.

Autor: Posiolova LV; Malin Space Science Systems, San Diego, CA, USA., Lognonné P; Université Paris Cité, Institut de Physique du Globe de Paris, CNRS, Paris, France., Banerdt WB; Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA, USA., Clinton J; Swiss Seismological Service, ETH Zurich, Zurich, Switzerland., Collins GS; Department of Earth Science and Engineering, Imperial College London, London, UK., Kawamura T; Université Paris Cité, Institut de Physique du Globe de Paris, CNRS, Paris, France., Ceylan S; Institute of Geophysics, ETH Zurich, Zurich, Switzerland., Daubar IJ; Department of Earth, Environmental, and Planetary Sciences, Brown University, Providence, RI, USA., Fernando B; Department of Earth Sciences, University of Oxford, Oxford, UK., Froment M; Université Paris Cité, Institut de Physique du Globe de Paris, CNRS, Paris, France.; Earth and Environmental Sciences Division, Los Alamos National Laboratory, Los Alamos, NM, USA., Giardini D; Institute of Geophysics, ETH Zurich, Zurich, Switzerland., Malin MC; Malin Space Science Systems, San Diego, CA, USA., Miljković K; Space Science and Technology Centre, School of Earth and Planetary Sciences, Curtin University, Perth, WA, Australia., Stähler SC; Institute of Geophysics, ETH Zurich, Zurich, Switzerland., Xu Z; Université Paris Cité, Institut de Physique du Globe de Paris, CNRS, Paris, France., Banks ME; NASA Goddard Space Flight Center, Greenbelt, MD, USA., Beucler É; Nantes Université, Université Angers, Le Mans Université, CNRS, UMR 6112, Laboratoire de Planétologie et Géosciences, Nantes, France., Cantor BA; Malin Space Science Systems, San Diego, CA, USA., Charalambous C; Department of Electrical and Electronic Engineering, Imperial College London, London, UK., Dahmen N; Institute of Geophysics, ETH Zurich, Zurich, Switzerland., Davis P; Department of Earth, Planetary, and Space Sciences, University of California, Los Angeles, CA, USA., Drilleau M; Institut Supérieur de l'Aéronautique et de l'Espace ISAE-SUPAERO, Toulouse, France., Dundas CM; U.S. Geological Survey, Astrogeology Science Center, Flagstaff, AZ, USA., Durán C; Institute of Geophysics, ETH Zurich, Zurich, Switzerland., Euchner F; Institute of Geophysics, ETH Zurich, Zurich, Switzerland., Garcia RF; Institut Supérieur de l'Aéronautique et de l'Espace ISAE-SUPAERO, Toulouse, France., Golombek M; Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA, USA., Horleston A; School of Earth Sciences, University of Bristol, Bristol, UK., Keegan C; Malin Space Science Systems, San Diego, CA, USA., Khan A; Institute of Geophysics, ETH Zurich, Zurich, Switzerland.; Physik-Institut, University of Zurich, Zurich, Switzerland., Kim D; Institute of Geophysics, ETH Zurich, Zurich, Switzerland.; Department of Geology, University of Maryland, College Park, MD, USA., Larmat C; Earth and Environmental Sciences Division, Los Alamos National Laboratory, Los Alamos, NM, USA., Lorenz R; Johns Hopkins Applied Physics Laboratory, Laurel, MD, USA., Margerin L; Institut de Recherche en Astrophysique et Planétologie, Université Toulouse III Paul Sabatier, CNRS, CNES, Toulouse, France., Menina S; Université Paris Cité, Institut de Physique du Globe de Paris, CNRS, Paris, France., Panning M; Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA, USA., Pardo C; Université Paris Cité, Institut de Physique du Globe de Paris, CNRS, Paris, France., Perrin C; Nantes Université, Université Angers, Le Mans Université, CNRS, UMR 6112, Laboratoire de Planétologie et Géosciences, Nantes, France., Pike WT; Department of Electrical and Electronic Engineering, Imperial College London, London, UK., Plasman M; Université Paris Cité, Institut de Physique du Globe de Paris, CNRS, Paris, France., Rajšić A; Space Science and Technology Centre, School of Earth and Planetary Sciences, Curtin University, Perth, WA, Australia., Rolland L; Université Côte d'Azur, Observatoire de la Côte d'Azur, CNRS, IRD, Géoazur, Valbonne, France., Rougier E; Earth and Environmental Sciences Division, Los Alamos National Laboratory, Los Alamos, NM, USA., Speth G; Malin Space Science Systems, San Diego, CA, USA., Spiga A; Laboratoire de Météorologie Dynamique/IPSL, Sorbonne Université, CNRS, Ecole Normale Supérieure, PSL Research University, Ecole Polytechnique, Paris, France., Stott A; Institut Supérieur de l'Aéronautique et de l'Espace ISAE-SUPAERO, Toulouse, France., Susko D; Malin Space Science Systems, San Diego, CA, USA., Teanby NA; School of Earth Sciences, University of Bristol, Bristol, UK., Valeh A; Malin Space Science Systems, San Diego, CA, USA., Werynski A; Malin Space Science Systems, San Diego, CA, USA., Wójcicka N; Department of Earth Science and Engineering, Imperial College London, London, UK., Zenhäusern G; Institute of Geophysics, ETH Zurich, Zurich, Switzerland.
Jazyk: angličtina
Zdroj: Science (New York, N.Y.) [Science] 2022 Oct 28; Vol. 378 (6618), pp. 412-417. Date of Electronic Publication: 2022 Oct 27.
DOI: 10.1126/science.abq7704
Abstrakt: Two >130-meter-diameter impact craters formed on Mars during the later half of 2021. These are the two largest fresh impact craters discovered by the Mars Reconnaissance Orbiter since operations started 16 years ago. The impacts created two of the largest seismic events (magnitudes greater than 4) recorded by InSight during its 3-year mission. The combination of orbital imagery and seismic ground motion enables the investigation of subsurface and atmospheric energy partitioning of the impact process on a planet with a thin atmosphere and the first direct test of martian deep-interior seismic models with known event distances. The impact at 35°N excavated blocks of water ice, which is the lowest latitude at which ice has been directly observed on Mars.
Databáze: MEDLINE
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