从布里格曼石的结晶学偏好方向推断出地幔动力学
Noriyoshi Tsujino1, Yu Nishihara2, Daisuke Yamazaki1
1Institute for Planetary Materials, Okayama University, 827 Yamada, Misasa, Tottori 682-0193, Japan.
Nature
|November 4, 2016
概括
布里格曼石
科学领域:
- 矿物物理
- 地震学
- 地动力学
背景情况:
- 在最上层的下层地幔中,地震剪切波的异形性与沉降板块有关.
- 布里格曼石的结晶偏向 (CPO) 是可能的原因,但其变形机制尚不清楚.
- 之前的研究确定了变形纹理,但不是主要的滑动系统.
研究的目的:
- 在最上下地幔条件下确定桥岩的主要滑动系统.
- 解释地震异性观测在沉积板块附近.
主要方法:
- 之前已经进行了单轴变形实验.
- 使用卡瓦伊型变形DIA装置进行了简单的剪切变形实验.
- 在25 GPa和1,873 K下分析了布里格曼酸CPO.
主要成果:
- 布里格曼石的主要滑动系统被确定为[001](100).
- CPO图案显示[100]垂直于剪切平面,并行于剪切方向.
- 这种CPO解释了加-克尔马德克,库里尔,秘鲁和爪等沉积板块附近的地震异性.
结论:
- [001](100) 滑动系统控制了最上层地幔的桥石变形.
- 由地幔流引起的布里格曼石CPO解释了观察到的地震异性.
- 这一发现提升了我们对地幔地力学和地震波传播的理解.
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