长期存在的月球火山活动是由前行驱动的核心-地幔摩擦所维持的
Shuoran Yu1, Xiao Xiao2, Shengxia Gong3
1State Key Laboratory of Lunar and Planetary Sciences, Macau University of Science and Technology, Macau 999078, China.
National science review
|January 12, 2024
概括
月球核心-地幔摩擦维持了早期地幔融化和火山活动. 这一过程也影响了月球核心的冷却和倾斜,可能增加了极地水冰沉积物.
科学领域:
- 行星科学 行星科学
- 地质物理学 地质物理学
- 月球科学 月球科学
背景情况:
- 月球旋转轴前行的核心-地幔摩擦是一个重要的早期热源.
- 它对月球热演变和地质活动的长期影响尚不清楚.
研究的目的:
- 为了研究核心-地幔摩擦对月球长期热演变的影响.
- 解释月球早期的火山活动及其对核心动态和水冰的影响.
- 模拟月球倾斜的演变及其对水分分配的影响.
主要方法:
- 利用一个一维的热进化模型.
- 模拟核心-地幔摩擦对地幔融和核心冷却的影响.
- 分析了卡西尼号状态的过渡及其对月球斜率的影响.
主要成果:
- 核心-地幔摩擦维持了上层地幔的全球部分融化,直到大约31亿年前.
- 这种摩擦抑制了长期的核心冷却,不太可能为长寿的月球动力发电机提供动力.
- 该模型支持卡西尼在月球岩海洋固化之前的状态过渡,表明月球倾斜度在固化后减少.
结论:
- 核心-地幔摩擦是解释早期月球火山活动的关键因素.
- 这些发现表明,对月球核心冷却和动力发电机潜力的理解有所改进.
- 月球斜率的下降可能会导致在极地地区更多的火山来源的水冰积累.
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