欧洲上的折叠:对地循环和扩展适应的影响
1Applied Physics Laboratory, Johns Hopkins University, MS 7-366, 11100 Johns Hopkins Road, Laurel, MD 20723, USA. louise.prockter@jhuapl.edu
概括
木星是木星,木星是木星,木星是木星.
科学领域:
- 行星科学 行星科学
- 地质地质地质地质地质地
- 地质物理学 地质物理学
背景情况:
- 木星的卫星欧洲表现出复杂的表面特征.
- 潮力量对欧洲的地质活动有很大的影响.
研究的目的:
- 调查欧洲地区范围波动的起源.
- 了解潮应力在欧洲地质演变中的作用.
主要方法:
- 分析区域规模的波动和相关的次要结构.
- 模拟由潮变形驱动的地质过程.
主要成果:
- 推断出的区域波动被解释为构造折叠.
- 折叠形成与来自潮压力的压缩不稳定性有关.
- 这些折叠可能是暂时的特征,以补偿扩展性构造学.
结论:
- 潮变形是欧洲上折叠形成的主要驱动因素.
- 欧罗巴的表面可能会经历周期性变形和放松.
- 了解这些折叠,可以深入了解内部海洋冰的相互作用.
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