太阳系II的小天体中的岩性过程:小卫星和矮行星
Giovanni Leone1,2, Hiroyuki Tanaka2,3,4
1Instituto de Investigación en Astronomía y Ciencias Planetarias, Universidad de Atacama, Copiapó 153000, Región de Atacama, Chile.
太阳系中小型天体显示出火热活动的证据,包括火山活动和冷火山活动. 像橄和火这样的矿物质表明过去的加热过程,可能是由放射性元素或潮力驱动的.
科学领域:
- 行星科学 行星科学
- 天文地质学 天文地质学
- 地质化学 地质化学
背景情况:
- 小卫星和矮行星都显示出火热和热水过程的证据.
- 这些天体的光谱检测了诸如橄和火素等矿物质.
- 塞雷斯和米兰达的奥利文 (蛇) 的水性变化表明内部的热水活动.
研究的目的:
- 调查小型太阳系天体中岩火和热水过程的流行和驱动因素.
- 了解原始加热和内部热源在塑造这些物体中的作用.
- 分析过去地质活动的矿物学证据.
主要方法:
- 小卫星和矮行星的光谱分析.
- 行星内部的地化学建模.
- 放射测年法和对同位素丰度 (例如26Al) 的分析.
主要成果:
- 检测到奥利文和烯表明火热的过程.
- 蛇形的存在表明水的变化和热水活动.
- 在太阳系早期无处不在的26Al提供了广泛的原始加热.
结论:
- 在小型太阳系天体中,火热和冷火山过程是常见的.
- 放射性元素的内部加热和潮力量是使火山活动成为可能的关键因素.
- 水热过程是由Ceres和Miranda等天体上的矿物学证据表明的.
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