矿后 (Mg,Fe) SiO3 的变形和 D' 的异构性
Sébastien Merkel1, Allen K McNamara, Atsushi Kubo
1Department of Earth and Planetary Science, University of California, Berkeley, CA 94720, USA. sebastien.merkel@univ-lille1.fr
在极端压力下,矿石后矿物质的塑性变形表明它们在特定的平面上滑动. 这影响了地球附近的地震异构性.
科学领域:
- 矿物物理 矿物物理
- 地力学是什么?地力学是什么?
- 地震学 地震学
背景情况:
- 矿后阶段在地球核心-地幔边界附近稳定.
- 了解其变形机制对于解释D'区域的地震异性质至关重要.
研究的目的:
- 在高压下研究矿后 (Mg{0.9},Fe{0.1}) SiO3 的塑性变形.
- 为了建模地球D'层中所产生的地震异构性.
主要方法:
- 塑料变形实验使用145-157 GPa的钻石天细胞进行.
- 使用对流和粘性塑性多晶可塑性模型进行塑料菌株和异构性的数值模拟.
主要成果:
- 格子偏好的方向表示在 (100) 和 (110) 平面上的主导滑动.
- 地震异构性显示出显著的深度依赖性,在下流板块转折点附近和之外发展.
- 计算的异构度对弹性模块敏感,难以与地震数据相协调.
结论:
- 矿后的塑性变形导致D'区域的地震异构.
- 取决于深度的异质性与下流板块动力学有关.
- 目前的模型难以与地震观测相匹配,原因是弹性模块的不确定性.
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