橄石聚合物的高剪切应变:风湿学和地震影响
M Bystricky1, K Kunze, L Burlini
1Geologisches Institut, ETH-Zentrum, 8092 Zürich, Switzerland. misha@erdw.ethz.ch
概括
高压实验揭示了橄烯聚合物的应变减弱,影响了上层地幔流动. 这种地震异构可能不会反映在再结晶的岩石中剪平面的方向.
科学领域:
- 地质物理学 地质物理学
- 矿物物理 矿物物理
- 构造学 构造学 构造学 构造学
背景情况:
- 奥利文的脱位爬行是地球上层地幔的一个关键变形机制.
- 在极端条件下了解橄树的行为对于地力学建模至关重要.
研究的目的:
- 为了研究在高压和高温扭曲下在橄烯聚合物中的应变减弱和再结晶.
- 评估这些过程对上层地幔流动和地震异性质的影响.
主要方法:
- 在高压和高温的扭转实验中对橄烯聚合物进行.
- 应变减弱,亚粒旋转再结晶和格子偏好的方向的分析.
主要成果:
- 在稳定状态变形之前观察到15-20%的应变减弱.
- 确定了亚粒旋转再结晶和强格子首选方向.
- 在高度紧张的地区,地震波的传播将是异构的.
结论:
- 应变减弱可能会促进上层地幔的流动,而不会改变变形机制.
- 基于低压力数据的现有流量规律对于高压力区域可能不足.
- 在高度应力,再结晶的橄中, anisotropy 不表明剪切平面的方向.
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