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月球Procellarum区域的结构和演变,由GRAIL重力数据揭示出来
Jeffrey C Andrews-Hanna1, Jonathan Besserer2, James W Head3
1Department of Geophysics and Center for Space Resources, Colorado School of Mines, Golden, Colorado 80401, USA.
Nature
|October 4, 2014
概括
在Procellarum地区.
科学领域:
- 月球地质学 月球地质学
- 地质物理学 地质物理学
- 星球科学 星球科学
背景情况:
- 月球近面的Procellarum区域的海拔较低,地薄,热生成元素度高.
- 以前的解释表明这是一个古老的冲击盆地,但表面证据被年龄和保存不佳所掩盖.
研究的目的:
- 通过使用来自重力恢复和内部实验室 (GRAIL) 任务的数据来检查Procellarum区域的地下结构.
- 重新评估Procellarum地区的地质起源.
主要方法:
- 来自GRAIL任务数据的Bouguer重力异常和重力梯度的分析.
- 由重力数据揭示的地下结构的解释.
主要成果:
- 格雷尔数据显示,Procellarum周围存在线性异常,被解释为古老的岩填充裂和堤.
- 这些结构形成了一个准矩形的图案,而不是撞击盆地的预期圆形形状.
- 以前被认为是冲击盆地边缘的表面特征是这种连续的岩石构造系统的一部分.
结论:
- 普罗塞拉鲁姆地区的边界结构起源于岩构造,而不是撞击盆地.
- 它们的形成与差异冷却和由高热流驱动的岩活动带来的热应力有关.
- 这为月球的火山和构造历史提供了新的见解.
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