由板宽控制的潜水区的演变和多样性
W P Schellart1, J Freeman, D R Stegman
1Research School of Earth Sciences, The Australian National University, Canberra, Australian Capital Territory 0200, Australia. wouter.schellart@anu.edu.au
Nature
|March 16, 2007
概括
石板宽度决定了俯冲区的形状和撤退速度. 狭窄的板块曲并迅速撤退,而宽的板块是静止和凸起的,影响板块构造和山脉形成.
科学领域:
- 地质物理学 地质物理学
- 构造学 构造学 构造学 构造学
- 地力学是什么?地力学是什么?
背景情况:
- 降温板块驱动板块运动和地幔流动.
- 之前的模型将俯冲区视为二维或空间固定.
- 现实潜伏区具有有限的,不断演变的3D几何形状.
研究的目的:
- 调查有限的板宽和几何如何影响俯冲区动态.
- 分析板块宽度,曲率和沟迁移之间的关系.
- 解释俯冲区退缩和构造特征观察到的全球变化.
主要方法:
- 自由潜伏的三维数值模拟.
- 模型板宽度的变化从250公里到超过4000公里.
- 将模拟结果与沟迁移和几何学的全球观测数据进行比较.
主要成果:
- 板宽度是潜伏区曲率和退缩的主要控制因素.
- 沟迁移率与板块宽度和板块边缘的距离成反比例.
- 狭窄的板块 (<1500公里) 迅速退缩,形成形几何形状;宽板块 (>4,000公里) 是静止和凸起的.
- 缓慢的沟前进发生在宽的板块中,这可能解释了安第斯山脉的形成.
结论:
- 有限的板块宽度从根本上塑造了俯冲区的演变和板块构造.
- 石边缘的接近对于理解快速的沟撤退至关重要.
- 沉浮板块的3D几何学提供了对大规模地质过程和特征的关键见解.
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