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Cratering and age of the small Saturnian satellites

机译:小型土星卫星的陨石坑和年龄

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Context. The small (≤135 km mean radius) satellites of Saturn are closely related to its rings and together they constitute a complex dynamical system where formation and destruction mechanisms compete against each other. The Cassini-Huygens mission provided high-resolution images of the surfaces of these satellites and therefore allowed for the calculation of observational crater counts. Aims. We model the cratering process by Centaur objects on the small Saturnian satellites, and compare our results with the observational crater counts obtained from the Voyager and Cassini missions. Methods. Using a theoretical model previously developed we calculate the crater production on these satellites considering two slopes of the size-frequency distribution (SFD) for the smaller objects of the Centaur population and compare our results with the available observations. In addition, we consider the case of catastrophic collisions between these satellites and Centaur objects and calculate the age of formation of those satellites that suffer one or more disruptions. Results. In general we find that the observed crater distributions are best modeled by the crater size distribution corresponding to the s _(2)= 3.5 index of the SFD of impactors with diameters smaller than 60 km. However, for crater diameters D ? 3 – 8 km (which correspond to impactor diameters d ~ 0.04 – 0.15 km), the observed distributions become flatter and deviate from our results, which may evidence processes of erosion and/or crater saturation at small crater sizes or a possible break in the SFD of impactors at d ~ 0.04 – 0.15 km to a much shallower differential slope of approximately ? 1.5. Our results suggest that Pan, Daphnis, Atlas, Aegaeon, Methone, Anthe, Pallene, Calypso, and Polydeuces suffered one or more catastrophic collisions over the age of the solar system, the younger being associated to arcs with ages of ~10~(8)yr. We have also calculated surface ages for the satellites, which indicate ongoing resurfacing processes.
机译:上下文。土星的小型卫星(平均半径≤135km)与其环密切相关,它们共同构成一个复杂的动力学系统,形成和破坏机制相互竞争。卡西尼-惠更斯飞行任务提供了这些卫星表面的高分辨率图像,因此可以用于计算观测的陨石坑计数。目的我们在小型土星卫星上模拟半人马座天体的陨石坑过程,并将我们的结果与从旅行者号和卡西尼号任务获得的观测陨石坑计数进行比较。方法。使用先前开发的理论模型,我们考虑了半人马座小型天体的大小-频率分布(SFD)的两个斜率,计算了这些卫星上的火山口产量,并将我们的结果与现有观测值进行了比较。此外,我们考虑了这些卫星与半人马座物体之间发生灾难性碰撞的情况,并计算了遭受一次或多次干扰的卫星的形成年龄。结果。总的来说,我们发现,观测到的火山口分布最好用对应于直径小于60 km的撞击器SFD的s_(2)= 3.5指数的火山口尺寸分布来建模。但是,对于弹坑直径D? 3 – 8 km(对应于撞击器直径d〜0.04 – 0.15 km),观察到的分布变得更平坦并且偏离我们的结果,这可能表明在小火山口尺寸下腐蚀和/或火山口饱和的过程,或火山口可能破裂。在d〜0.04 – 0.15 km处,冲击器的SFD到大约更浅的微分斜率? 1.5。我们的研究结果表明,Pan,Daphnis,Atlas,Aegaeon,Methone,Anthe,Pallene,Calypso和Polydeuces在太阳系的整个寿命中遭受了一次或多次灾难性碰撞,年轻的是与〜10〜(8 )年。我们还计算了卫星的表面年龄,这表明正在进行的重铺过程。

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