地岩石的快速粘性流控制着地层在柔性地中的堤位置
Hans Jørgen Kjøll1, Thomas Scheiber2, Olivier Galland3
1Njord centre, Department of Geosciences, University of Oslo, Oslo, Norway. h.j.kjoll@geo.uio.no.
Nature communications
|December 23, 2025
概括
深层地的岩堤造成了宿主岩石的显著延展性变形,这与之前的假设相反. 这一发现影响了我们对地强度和地缘危险评估的理解.
科学领域:
- 地球科学 地球科学 地球科学
- 地质地质地质地质地质地
- 构造学 构造学 构造学 构造学
背景情况:
- 岩堤是岩通过地球地上升的主要通道.
- 堤位通常被建模为具有弹性宿主岩石曲的拉力断裂传播.
研究的目的:
- 为了研究与深层地堤位置相关的变形机制.
- 在堤入侵过程中量化宿主岩中软性变形的作用.
主要方法:
- 在瑞典北部对堤与宿主岩石相互作用的现场观测.
- 对柔性变形特征和厚度适应的分析.
- 模拟岩冷却时间以估计应变速率.
主要成果:
- 在与堤相邻的宿主岩石中观察到显著的柔性变形,占堤厚度的25%.
- 估计的柔性拉伸速率 (10^-3到10^-6s^-1) 比典型的构造速率高出数量级.
- 证据挑战了深层地层堤安置的纯脆裂纹模型.
结论:
- 深层地堤位包括大量的柔性宿主岩石流.
- 这些发现需要修订地强度和岩运输模型.
- 改进的理解有助于解释地质信号以缓解地质危险.
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