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The topography of Iapetus' leading side

Giese, Bernd und Denk, Tilmann und Neukum, Gerhard und Roatsch, Thomas und Helfenstein, Paul und Thomas, Peter und Turtle, Elizabeth und McEwen, Alfred und Porco, Carolyn (2008) The topography of Iapetus' leading side. Icarus, 193 (2), Seiten 359-371. Elsevier. DOI: 10.1016/j.icarus.2007.06.005

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We have used Cassini stereo images to study the topography of Iapetus' leading side. A terrain model derived at resolutions of 4-8 km reveals that Iapetus has substantial topography with heights in the range of -10 km to +13 km, much more than observed on the other middle-sized satellites of Saturn so far. Most of the topography is older than 4 Ga (Neukum et al., 2005) which implies that Iapetus must have had a thick lithosphere early in its history to support this topography. Models of lithospheric deflection by topographic loads provide an estimate of the required elastic thickness in the range of 50-100 km. Iapetus' prominent equatorial ridge (Porco et al., 2005) reaches widths of 70 km and heights of up to 13 km from their base within the modeled area. The morphology of the ridge suggests an endogenous origin rather than a formation by collisional accretion of a ring remnant (Ip, 2006). The transition from simple to complex central peak craters on Iapetus occurs at diameters of 11±3 km. The central peaks have pronounced conical shapes with flanking slopes of typically 11° and heights that can rise above the surrounding plains. Crater depths seem to be systematically lower on Iapetus than on similarly sized Rhea, which if true, may be related to more pronounced crater-wall slumping (which widens the craters) on Iapetus than on Rhea. There are seven large impact basins with complex morphologies including central peak massifs and terraced walls, the largest one reaches 800 km in diameter and has rim topography of up to 10 km. Generally, no rings are observed with the basins consistent with a thick lithosphere but still thin enough to allow for viscous relaxation of the basin floors, which is inferred from crater depth-to-diameter measurements. In particular, a 400-km basin shows up-domed floor topography which is suggestive of viscous relaxation. A model of complex crater formation with a viscoplastic (Bingham) rheology (Melosh, 1989) of the impact-shocked icy material provides an estimate of the effective cohesion / viscosity at 0.04±0.01 MPa / 0.6±0.2 GPas. The local distribution of bright and dark material on the surface of Iapetus is largely controlled by topography and consistent with the dark material being a sublimation lag deposit originating from a bright icy substrate mixed with the dark components, but frost deposits are possible as well.

Titel:The topography of Iapetus' leading side
AutorenInstitution oder E-Mail-AdresseAutoren-ORCID
Denk, TilmannFreie Universität BerlinNICHT SPEZIFIZIERT
Neukum, GerhardFreie Universität BerlinNICHT SPEZIFIZIERT
Helfenstein, PaulCornell University, Ithaca, USANICHT SPEZIFIZIERT
Thomas, PeterCornell University, Ithaca, USANICHT SPEZIFIZIERT
Turtle, ElizabethJohns Hopkins University, Laurel, USANICHT SPEZIFIZIERT
McEwen, AlfredUniversity of Arizona, Tucson, USANICHT SPEZIFIZIERT
Porco, CarolynSpace Science Institute, Boulder, USANICHT SPEZIFIZIERT
Erschienen in:Icarus
In Open Access:Nein
In ISI Web of Science:Nein
DOI :10.1016/j.icarus.2007.06.005
Seitenbereich:Seiten 359-371
Stichwörter:Iapetus, Saturn satellites, Craters
HGF - Forschungsbereich:Verkehr und Weltraum (alt)
HGF - Programm:Weltraum (alt)
HGF - Programmthema:W EW - Erforschung des Weltraums
DLR - Schwerpunkt:Weltraum
DLR - Forschungsgebiet:W EW - Erforschung des Weltraums
DLR - Teilgebiet (Projekt, Vorhaben):W - Vorhaben CASSINI (alt)
Standort: Berlin-Adlershof
Institute & Einrichtungen:Institut für Planetenforschung > Planetengeodäsie
Institut für Planetenforschung > Planetengeologie
Hinterlegt von: Giese, Dr.rer.nat. Bernd
Hinterlegt am:26 Jan 2009
Letzte Änderung:07 Aug 2017 10:43

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