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月球的金牛座-利特罗山谷的古地震活动是由巨石落和山体滑坡推断的
Thomas R Watters1, Nicholas C Schmerr2
1Smithsonian Institution, Washington, DC, USA.
塔鲁斯-利特罗山谷的月球地震造成了山体滑坡和巨石塌. 对阿波罗17号样本的分析表明,这些来自李-林肯推力断层的地震事件是强大而浅的,对未来的月球任务构成危险.
科学领域:
- 月球地质学 月球地质学
- 地震学 地震学
- 星球科学 星球科学
背景情况:
- 金牛座-利特罗谷提供了一个独特的自然实验室来研究月球表面的变化.
- 地震活动,特别是月球地震,已经通过诸如山体滑坡和巨石落等事件显然改变了景观.
- 李-林肯推力断层是该地区月球地震的可能来源.
研究的目的:
- 为了估计金牛座-利特罗山谷特定地质特征的地面加速和月球地震强度.
- 用月球样本的曝光年龄来确定月球地震的时间.
- 评估月球地震活动对未来勘探的影响.
主要方法:
- 在阿波罗17号任务期间采集的地质特征 (巨石,山体滑坡) 的分析.
- 估计地面加速和地震事件的大小.
- 用暴露年龄来约定地质特征的年代,以限制月球地震的时间.
主要成果:
- 分析了塔乌罗斯-利特罗山谷的四块巨石和一个山体滑坡.
- 李-林肯断层的结构浮雕归因于多次共震滑动事件.
- 对于这些事件,估计的最小体波大小 (Mw) 范围大约在2.9至3.3.之间.
结论:
- 月球在其历史上经历了广泛,强烈,浅的月球地震.
- 许多年轻推力断层的形成和生长表明过去的地震活动显著.
- 来自活跃断层的浅层月球地震对长期的月球前哨站构成潜在的危险.
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