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Scattering And Absorption of Light in Planetary Regoliths
Published on: July 1, 2019
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在小行星4维斯塔上有一个深层地-地幔边界
Harold Clenet1, Martin Jutzi2, Jean-Alix Barrat3
1EPSL, Institute of Condensed Matter Physics, Ecole Polytechnique Fédérale de Lausanne (EPFL), Station 3, CH-1015 Lausanne, Switzerland.
Nature
|July 18, 2014
概括
小行星维斯塔 (Vesta) 的存在.
科学领域:
- 行星科学 行星科学
- 小行星研究研究.
- 地质物理学 地质物理学
背景情况:
- 小行星4 Vesta在其南极附近展现了两个大型撞击坑.
- 这些石坑暴露了地下物质,为维斯塔的内部结构提供了洞察力.
- 之前的建模表明,维斯塔半球表面材料的深度不同.
研究的目的:
- 分析来自小行星4 Vesta的数据.
- 为了确定维斯塔的地和地幔边界 (Moho) 的深度.
- 为了研究维斯塔的外层的组成.
主要方法:
- 对小行星4 Vesta.撞击坑数据的分析.
- 地下物质暴露的建模.
- 对维斯塔的结构进行地质物理解释.
主要成果:
- 维斯塔北半球的表面材料起源于~20公里的深度.
- 暴露的南方材料来自60-100公里的深度.
- 没有显著的橄石表明,外面的100公里主要是火热地.
结论:
- 小行星4维斯塔的地-地幔边界 (Moho) 深度超过80公里.
- 维斯塔的外层主要由火性地组成.
- 撞击事件为了解小行星内部提供了关键数据.
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