融化分离和应变分离:对地震异构性和地幔流量的影响
B K Holtzman1, D L Kohlstedt, M E Zimmerman
1Department of Geology and Geophysics, University of Minnesota, Minneapolis, MN 55455, USA. holtz007@umn.edu
概括
在地球上层地幔中融化的存在影响了地震异构性. 地震快速方向,通常与流动平行,当融化形成弱区时,可以从剪切方向上取向90度,改变我们解释地幔动态的方式.
科学领域:
- 地质物理学 地质物理学
- 地震学 地震学
- 固体地球科学 固体地球科学
背景情况:
- 了解上层地幔的动力学依赖于地震异构性解释.
- 假设地震快速方向与区域地幔流平行.
- 奥利文的a轴方向是地震快速方向的关键.
研究的目的:
- 调查融存在和分离对地震异性质的影响.
- 重新评估在部分化地区的地震快速方向和地幔流动之间的关系.
主要方法:
- 这项研究理论上检查了融对奥利文a轴对齐的影响.
- 它使用分离的融网络建模三维变形.
- 分析了弱区和强区之间的应变分区.
主要成果:
- 化的存在削弱了橄烯a轴的对齐.
- 分离融化形成弱剪切区域导致a轴与剪切方向90度的对齐.
- 这表明在部分化的地幔中存在应变分离.
结论:
- 在部分化区域中,直接指示流动方向的地震快速方向假设受到挑战.
- 对于变形,部分化的地球区域,提出了地震异构的新解释.
- 这一发现为上层地幔流动动力学提供了新的见解.
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