奥利文晶体在地球上层地幔的扩散爬行过程中对齐
Tomonori Miyazaki1, Kenta Sueyoshi, Takehiko Hiraga
1Earthquake Research Institute, University of Tokyo, 1-1-1 Yayoi, Bunkyo-ku, Tokyo 113-0032, Japan.
Nature
|October 18, 2013
概括
扩散爬行,而不仅仅是脱位爬行,可以创建橄晶体对齐. 这一发现影响了我们对地幔流动和地球上层地幔的地震异性质的理解.
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:
- 橄石的结晶学偏好方向 (CPO) 对于理解地球上层地幔的异构和流动至关重要.
- 脱位爬行是传统上被接受的产生橄CPO的机制.
研究的目的:
- 调查扩散爬行是否也可以在橄中产生CPO.
- 为了确定温度和融对在扩散爬行过程中CPO发展的影响.
主要方法:
- 在不同温度和融化条件下,无铁的橄烯 (石) 的实验变形.
- 分析得到的结晶学偏好方向 (CPO) 模式.
主要成果:
- 扩散爬行在石中产生CPO,其模式取决于温度和融的存在.
- CPO强度与温度和融化相关,影响谷物边界特征和滑动.
- 预测的地震异质性模式与观测到的辐射异质性和上层地幔的地震速度变化保持一致.
结论:
- 扩散爬行是产生奥利文CPO和地幔异性质的一个重要机制.
- 拟议的扩散爬行模型解释了不同地幔温度调节的地震观测.
- 这挑战了仅仅依赖脱位爬行来解释地幔流动来自地震异性质的挑战.
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