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土卫十八(潘)和土卫十五(阿特拉斯)的赤道脊:终端增生饰纹?

The equatorial ridges of Pan and Atlas: terminal accretionary ornaments?

作者信息

Charnoz Sébastien, Brahic André, Thomas Peter C, Porco Carolyn C

机构信息

Laboratoire AIM, Commissariat à l'Energie Atomique (CEA)/Université Paris 7/CNRS, 91191 Gif-sur-Yvette Cedex, France.

出版信息

Science. 2007 Dec 7;318(5856):1622-4. doi: 10.1126/science.1148631.

Abstract

In the outer regions of Saturn's main rings, strong tidal forces balance gravitational accretion processes. Thus, unusual phenomena may be expected there. The Cassini spacecraft has recently revealed the strange "flying saucer" shape of two small satellites, Pan and Atlas, located in this region, showing prominent equatorial ridges. The accretion of ring particles onto the equatorial surfaces of already-formed bodies embedded in the rings may explain the formation of the ridges. This ridge formation process is in good agreement with detailed Cassini images showing differences between rough polar and smooth equatorial terrains. We propose that Pan and Atlas ridges are kilometers-thick "ring-particle piles" formed after the satellites themselves and after the flattening of the rings but before the complete depletion of ring material from their surroundings.

摘要

在土星主环的外部区域,强大的潮汐力平衡着引力吸积过程。因此,预计那里会出现异常现象。卡西尼号航天器最近揭示了位于该区域的两颗小卫星——土卫十四和土卫十五呈现出奇怪的“飞碟”形状,并显示出明显的赤道脊。环粒子在嵌入环中的已形成天体的赤道表面上的吸积可能解释了这些脊的形成。这一脊形成过程与卡西尼号的详细图像非常吻合,这些图像显示了粗糙的极地地形和平滑的赤道地形之间的差异。我们认为,土卫十四和土卫十五的脊是在卫星自身形成、环变得扁平之后,但在其周围的环物质完全耗尽之前形成的数公里厚的“环粒子堆积”。

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