Surface ages of mid-size Saturnian satellites

The observations of the surfaces of the mid-sized saturnian satellites made by Cassini–Huygens mission have shown a variety of features that allows study of the processes that took place and are taking place on those worlds. Research of the saturnian satellite surfaces has clear implications not onl...

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Autores principales: Di Sisto, Romina Paula, Zanardi, Macarena
Formato: Articulo Preprint
Lenguaje:Inglés
Publicado: 2016
Materias:
Acceso en línea:http://sedici.unlp.edu.ar/handle/10915/93618
https://www.sciencedirect.com/science/article/pii/S0019103515004157?via%3Dihub
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id I19-R120-10915-93618
record_format dspace
institution Universidad Nacional de La Plata
institution_str I-19
repository_str R-120
collection SEDICI (UNLP)
language Inglés
topic Ciencias Astronómicas
Saturn
Cratering
Centaurs
Stellites
spellingShingle Ciencias Astronómicas
Saturn
Cratering
Centaurs
Stellites
Di Sisto, Romina Paula
Zanardi, Macarena
Surface ages of mid-size Saturnian satellites
topic_facet Ciencias Astronómicas
Saturn
Cratering
Centaurs
Stellites
description The observations of the surfaces of the mid-sized saturnian satellites made by Cassini–Huygens mission have shown a variety of features that allows study of the processes that took place and are taking place on those worlds. Research of the saturnian satellite surfaces has clear implications not only for Saturn’s history and Saturn’s surroundings, but also for the Solar System. Crater counting from high definition images is very important and could serve for the determination of the age of the surfaces. In a recent paper, we have calculated the production of craters on the mid-sized saturnian satellites by Centaur objects considering the current configuration of the Solar System. Also, we have compared our results with crater counts from Cassini images by other authors and we have noted that the number of observed small craters is less than our calculated theoretical number. In this paper we estimate the age of the surface for each observed terrain on each mid-sized satellite of Saturn. All the surfaces analyzed appear to be old with the exception of Enceladus. However, we have noticed that since there are less observed small craters than calculated (except on Iapetus), this results in younger ages than expected. This could be the result of efficient endogenous or exogenous process(es) for erasing small craters and/or crater saturation at those sizes. The size limit from which the observed number of smaller craters is less than the calculated is different for each satellite, possibly indicating processes that are unique to each, but other potential common explanations for this paucity of small craters would be crater saturation and/or deposition of E-ring particles. These processes are also suggested by the findings that the smaller craters are being preferentially removed, and the erasure process is gradual. On Enceladus, only mid and high latitude plains have remnants of old terrains; the other regions could be young. In particular, the regions near the South Polar Terrain could be as young as 50 Myr old. On the contrary for Iapetus, all the surface is old and it notably registers a primordial source of craters. As the crater size is decreased, it would be perceived to approach saturation until DK 2 km-craters, where saturation is complete.
format Articulo
Preprint
author Di Sisto, Romina Paula
Zanardi, Macarena
author_facet Di Sisto, Romina Paula
Zanardi, Macarena
author_sort Di Sisto, Romina Paula
title Surface ages of mid-size Saturnian satellites
title_short Surface ages of mid-size Saturnian satellites
title_full Surface ages of mid-size Saturnian satellites
title_fullStr Surface ages of mid-size Saturnian satellites
title_full_unstemmed Surface ages of mid-size Saturnian satellites
title_sort surface ages of mid-size saturnian satellites
publishDate 2016
url http://sedici.unlp.edu.ar/handle/10915/93618
https://www.sciencedirect.com/science/article/pii/S0019103515004157?via%3Dihub
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