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从GRAIL引力数据中揭示了月球Oceanus Procellarum区域下面的岩结构和连接性
Meixia Geng1, Qingjie Yang2, Chaouki Kasmi2
1Directed Energy Research Centre, Technology Innovation Institute, Abu Dhabi, United Arab Emirates. meixia.geng@tii.ae.
Nature communications
|November 28, 2024
概括
月球火山结构的密度模型揭示了在Oceanus Procellarum下方相互连接的岩管道. 这些路径促进了岩的运输,塑造了月球的火山历史.
科学领域:
- 月球地质学 月球地质学
- 星球上的火山活动.
- 地质物理学 地质物理学
背景情况:
- 海洋前 (Oceanus Procellarum) 展现了广的玄武岩平原和显著的火山活动.
- 了解月球火山历史需要详细调查地下岩系统.
研究的目的:
- 为了模拟海洋前 (Oceanus Procellarum) 下的岩结构的密度.
- 研究月球火山系统的连接和结构.
主要方法:
- 利用了来自重力恢复和内部实验室 (GRAIL) 任务的数据.
- 开发了地下岩结构的密度模型.
主要成果:
- 在Procellarum西部边界沿线确定了线性岩结构.
- 在马里乌斯山丘的北部和南部发现了大量的入侵.
- 发现了连接这些入侵的三个近水平的板状岩管道 (长80-150公里,深6-7公里).
结论:
- 发现的管道充当了横向岩运输的中心通道.
- 在Oceanus Procellarum下方展示了广泛的岩连接.
- 突出了在月球火山演化中的横向运输的重要性.
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