The Margaritifer-Meridiani-Arabia highlands-lowlands (H-L) transition has long been recognized as the most fluvially dissected region of Mars. However, the geomorphic evolution of this region remains enigmatic, particularly the origin of the layered deposits of Meridiani Terra and Arabia. We suggest that a portion of this regional slope served as a fluvial depositional platform during the late Noachian.


    Zugriff

    Zugriff über TIB

    Verfügbarkeit in meiner Bibliothek prüfen


    Exportieren, teilen und zitieren



    Titel :

    A Sedimentary Platform in Margaritifer Sinus, Meridiani Terra, and Arabia?


    Beteiligte:
    Howard, A. D. (Autor:in) / Moore, J. M. (Autor:in) / Irwin, R. P., III (Autor:in) / Craddock, R. A. (Autor:in)


    Erscheinungsdatum :

    2005-01-01


    Medientyp :

    Aufsatz (Konferenz)


    Format :

    Keine Angabe


    Sprache :

    Englisch