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hal.structure.identifierBrigham Young University [BYU]
dc.contributor.authorRADEBAUGH, Jani
hal.structure.identifierUniversiteit Utrecht / Utrecht University [Utrecht]
dc.contributor.authorVENTRA, Dario
hal.structure.identifierJohns Hopkins University Applied Physics Laboratory [Laurel, MD] [APL]
dc.contributor.authorLORENZ, Ralph
hal.structure.identifierJet Propulsion Laboratory [JPL]
dc.contributor.authorFARR, Tom
hal.structure.identifierAstrogeology Science Center [Flagstaff]
dc.contributor.authorKIRK, Randy
hal.structure.identifierDepartment of Astronomy [Ithaca]
dc.contributor.authorHAYES, Alex
hal.structure.identifierJet Propulsion Laboratory [JPL]
dc.contributor.authorMALASKA, Michael
hal.structure.identifierDepartment of Astronomy [Ithaca]
dc.contributor.authorBIRCH, Sam
hal.structure.identifierSchool of Earth and Space Exploration [Tempe] [SESE]
dc.contributor.authorLIU, Zac Yung-Chun
hal.structure.identifierDepartment of Astronomy [Ithaca]
dc.contributor.authorLUNINE, Jonathan
hal.structure.identifierUniversity of Idaho [Moscow, USA]
dc.contributor.authorBARNES, Jason
hal.structure.identifierPLANETO - LATMOS
dc.contributor.authorLE GALL, Alice
hal.structure.identifierJet Propulsion Laboratory [JPL]
dc.contributor.authorLOPES, Rosaly
hal.structure.identifierProxemy Research Inc
dc.contributor.authorSTOFAN, Ellen
hal.structure.identifierJet Propulsion Laboratory [JPL]
dc.contributor.authorWALL, Steve
hal.structure.identifierASP 2015
hal.structure.identifierLaboratoire d'Astrophysique de Bordeaux [Pessac] [LAB]
dc.contributor.authorPAILLOU, Philippe
dc.date.issued2018-06-11
dc.identifier.issn2041-4927
dc.description.abstractEnFans, landforms that record the storage and transport of sediment from uplands to depositional basins, are found on Saturn's moon Titan, a body of significantly different process rates and material compositions from Earth. Images obtained by the Cassini spacecraft's synthetic aperture radar reveal morphologies, roughness, textural patterns and other properties consistent with fan analogues on Earth also viewed by synthetic aperture radar. The observed fan characteristics on Titan reveal some regions of high relative relief and others with gentle slopes over hundreds of kilometres, exposing topographic variations and influences on fan formation. There is evidence for a range of particle sizes across proximal to distal fan regions, from c. 2 cm or more to fine-grained, which can provide details on sedimentary processes. Some features are best described as alluvial fans, which implies their proximity to high-relief source areas, while others are more likely to be fluvial fans, drawing from larger catchment areas and frequently characterized by more prolonged runoff events. The presence of fans corroborates the vast liquid storage capacity of the atmosphere and the resultant episodic behaviour. Fans join the growing list of landforms on Titan derived from atmospheric and fluvial processes similar to those on Earth, strengthening comparisons between these two planetary bodies.
dc.language.isoen
dc.publisherGeological Society of London
dc.title.enAlluvial and fluvial fans on Saturn's moon Titan reveal processes, materials and regional geology
dc.typeArticle de revue
dc.identifier.doi10.1144/SP440.6
dc.subject.halPlanète et Univers [physics]/Astrophysique [astro-ph]
bordeaux.journalThe Geological Society, London, Special Publications
bordeaux.page281-305
bordeaux.volume440
bordeaux.issue1
bordeaux.peerReviewedoui
hal.identifierhal-02973057
hal.version1
hal.popularnon
hal.audienceInternationale
hal.origin.linkhttps://hal.archives-ouvertes.fr//hal-02973057v1
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