澳大利亚板块漂移的快速变化记录了与通爪高原的碰撞
Kurt M Knesel1, Benjamin E Cohen, Paulo M Vasconcelos
1Earth Sciences, The University of Queensland, St Lucia, Queensland, 4072, Australia. k.knesel@uq.edu.au
Nature
|August 8, 2008
概括
在通爪高原.
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.
- 地质时间学 (Geochronology)
背景情况:
- 海洋高原,如通爪高原,影响板块运动模型.
- 了解它们的沉降历史是板块重组的关键.
- 之前的研究缺乏对通爪高原美拉尼西亚沟碰撞的精确时间.
研究的目的:
- 解读通爪高原与澳大利亚板块之间的碰撞历史.
- 为了评估海洋高原沉降对板块运动的影响.
- 为了限制通爪高原到达美拉尼西亚沟的时间.
主要方法:
- (40) 澳大利亚东部火山热点的地质年代测算.
- 塔斯曼海海底山脉链轨道偏移的分析.
- 地质年代数据与板块运动模型的相关性.
主要成果:
- 新的地球时间学数据揭示了通爪高原碰撞与澳大利亚板块运动之间的联系.
- 确定了短暂的北向板块运动减少的时期 (26-23万年前).
- 澳大利亚板块在高原进入美拉尼西亚沟时向西偏移的证据.
结论:
- 通爪高原与美拉尼西亚弧线的碰撞导致澳大利亚板块短暂向西倾斜.
- 这一事件发生在26万年前,在特罗布里安德谷沿着西南方向的沉降开始.
- 巨大的海洋高原可以引发巨大的,全球范围的变化板边界和运动.
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