非洲热点火山活动:在 Kratons 下的上层地幔中小规模的对流
1Department of Earth and Atmospheric Sciences, Purdue University, West Lafayette, IN 47907-1397, USA. sking@purdue.edu
概括
上层地幔的小规模对流解释了非洲和南美洲下面的板块内火山活动和地震异常. 边缘驱动的对流为理解这些地质特征提供了地幔羽毛的替代方案.
科学领域:
- 地质物理学 地质物理学
- 地力学是什么?地力学是什么?
- 地幔对流对流是地幔的对流.
背景情况:
- 非洲和南美洲的内部火山活动和地震异常构成了地质难题.
- 地幔羽毛一直是主要假设,但人们正在寻求其他解释.
研究的目的:
- 为了研究小规模对流在上层地幔中的作用.
- 为了解释板内部火山活动的起源和在克拉顿和海洋石灰岩层下面的地震特征.
主要方法:
- 对地幔对流的数值建模.
- 在厚厚的岩板和薄薄的海洋板之间对石层过渡的分析.
主要成果:
- 小规模的对流在厚厚的岩层和薄薄的海洋岩层之间的边界上发展.
- 模型成功地复制了板内火山的位置和地化学特征.
- 高地震剪波速度 (冷下流) 与模型预测是一致的.
结论:
- 小规模,边缘驱动的对流提供了一个可行的替代地幔羽毛解释板内火山活动.
- 这种对流模式与在非洲和南美洲石化层下方观察到的地幔下层相一致.
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