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在过渡区的全球亚齐特异性
Jeannot Trampert1, Hendrik Jan van Heijst
1Faculty of Earth Sciences, Utrecht University, Post Office Box 80021, 3508 TA Utrecht, Netherlands. jeannot@geo.uu.nl
概括
爱的波浪外调揭示了地球上的亚齐木斯特异性.
科学领域:
- 地质物理学 地质物理学
- 地震学 地震学
- 地球科学 地球科学 地球科学
背景情况:
- 地球地幔过渡区 (深度400-660公里) 在地幔动力学和化学循环中起着至关重要的作用.
- 了解物理属性,如地震异构性,是限制该区域模型的关键.
- 亚齐穆特异性,地震波速度的方向变化,提供了对首选矿物质定向或纹理织物的洞察.
研究的目的:
- 为了研究地球地幔过渡区内亚齐木斯特异性存在和特征.
- 利用表面波分散数据,在这些深度探测地震速度结构.
- 根据观察到的异构性,为过渡区的矿物学和动态提供新的约束.
主要方法:
- 对表面波散射测量的分析,特别关注爱情波的共.
- 应用Backus-Gilbert反转技术到异构相位速度图.
- 确保分辨率内核主要对过渡区 (400-660公里深) 敏感.
主要成果:
- 在过渡区中检测到显著的亚齐木斯特异性证据.
- 确定了一种强大的,长波长的近距离离心异型速度结构.
- 逆转成功地在目标深度范围内绘制了这些异构特征.
结论:
- 在过渡区观察到的亚齐木斯特异性对理解其构成和变形具有重要意义.
- 这种异构的潜在来源包括对齐的矿物质,倾斜的层状结构或流体内含物.
- 这些发现为地幔过渡区的地力学和矿物物理模型提供了新的约束.
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