在冰岛Bárðarbunga火山系统的裂变事件中,分段横向堤的增长,冰岛
Freysteinn Sigmundsson1, Andrew Hooper2, Sigrún Hreinsdóttir3
1Nordic Volcanological Center, Institute of Earth Sciences, University of Iceland, IS-101 Reykjavík, Iceland.
Nature
|December 18, 2014
概括
一个细分的堤入侵延伸超过45公里,受地形和压力积累的影响,证明了在分离板块边界形成地的新机制.
科学领域:
- 地质物理学 地质物理学
- 火山学 火山学是一门学科.
- 构造学 构造学 构造学 构造学
背景情况:
- 在不同板块边界的地形成通常涉及垂直板状堤.
- 之前的模型对地形学在横向堤演变中的作用缺乏清晰度.
研究的目的:
- 为了研究细分堤入侵的横向生长.
- 了解地形和压力对堤传播的影响.
- 阐明在不同板块边界上层地形成的机制.
主要方法:
- 传播地震性和地面变形的分析 (全球定位系统).
- 卫星雷达图像的干涉度分析 (InSAR).
- 开发一种最小化应变和重力潜在能量的模型.
主要成果:
- 一个细分的堤在14天内横向侵入了45公里,传播速度可变.
- 地形影响了堤传播方向;压力积累克服了细分障碍.
- 堤的演变与火山口的膨胀,崩和地震活动相吻合.
结论:
- 侧面堤增长与断段障碍破裂解释了岩再分配的地形成.
- 这一过程有效地在不同的板块边界形成了新的上层地.
- 地形和内部压力是堤传播动态的关键因素.
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