地球上层地幔的温和到野性的可塑性
David Wallis1, Kathryn M Kumamoto2, Thomas Breithaupt1
1Department of Earth Sciences, University of Cambridge, Cambridge, UK.
概括
地球的上层地幔可能不会连续流动. 新的研究表明,一个主要的地幔矿物质奥利文,呈现间歇性的"野生"塑料流,这表明更深的地幔变形可能比以前认为的更为动态.
科学领域:
- 地质物理学 地质物理学
- 材料科学 材料科学 材料科学
- 矿物物理 矿物物理
背景情况:
- 地球上层地幔的流动传统上被建模为缓慢的,连续的爬行.
- 高分辨率实验显示,材料表现出一系列的塑性行为,从温和到野生.
研究的目的:
- 为了研究不同条件下的橄烯的塑性行为.
- 为了确定橄石在其塑性变形中是否表现出"野性".
主要方法:
- 在室温下对橄单晶进行纳米印记实验.
- 分析塑料应变速率波动和位移爆发的分析.
主要成果:
- 奥利文在塑料流中显示出可测量的"野性",即使在温和的条件下.
- 间歇性的位移爆发,表明位移雪崩,占塑料应变的8%左右.
- 这些爆发遵循日志常态分布,这是雪崩现象的特征.
结论:
- 这项研究证明了橄石的间歇性可塑性,挑战了上层地幔流量的连续爬行模型.
- 温和到野性的可塑性框架表明,随着深度的增加,"野性"会增加,从而影响天气层的变形.
- 这些发现为失位介导的流量模型提供了新的约束,并提出了诸如深度地震和缓慢滑动事件等暂时不稳定的问题.
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