扩大山脊迁移,这是由羽毛状山脊脱所实现的
Ben Mather1, Maria Seton2, Simon Williams3
1EarthByte Group, School of Geosciences, The University of Sydney, Sydney, NSW, Australia. ben.mather@sydney.edu.au.
Nature communications
|October 16, 2024
概括
地幔羽毛可以定或解,扩展山脊. 高浮力流量羽毛 (>3000公斤/秒) 稳定了山脊,而减弱的流量 (<1000公斤/秒) 可以导致快速迁移,影响板块构造.
科学领域:
- 地质物理学 地质物理学
- 板块构造学是一种板块构造学.
- 地幔动力学地幔动力学
背景情况:
- 扩散的脊主要受到俯冲力和不对称的应变速率的影响,这解释了它们的迁移.
- 地幔羽毛在板块边界的演变和蔓延山脊动态中的作用尚不清楚.
研究的目的:
- 为了研究地幔羽毛对扩散山脊的定和迁移的影响.
- 探索羽毛山丘脱的机制及其对板块构造学的影响.
主要方法:
- 利用地幔对流的数值模型来模拟羽毛-相互作用.
- 分析不同羽毛浮力流量对蔓延山脊稳定性的影响.
主要成果:
- 高浮力流层羽毛 (>3000 kg/s) 可以捕获和定 1000 公里半径内的蔓延山脊.
- 衰落的羽毛浮力流 (<1000公斤/秒) 可以解除山脊的,这与不对称的板块力量相结合时导致快速迁移.
- 异常高的浮力流可能会使覆盖板块碎片化,从而增强板块运动.
结论:
- 羽毛-山脊脱是影响板块边界演变的重要机制,正如西南印度山脊和Kerguelen羽毛可能观察到的那样.
- 这种机制对了解板块运动和地幔羽毛附近区域的动态有全球影响.
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