大型外星撞击造成的动态断裂是破碎的起源
Amir Sagy1, Ze'ev Reches, Jay Fineberg
1Institute of Earth Sciences, The Hebrew University of Jerusalem, 91904 Jerusalem, Israel.
Nature
|July 19, 2002
概括
撞击会产生破碎圆,这是有条纹特征的变形岩石. 新的研究表明,这些条纹是由沿断层传播的非线性波浪形成的,这解释了它们在撞击地点的形成和分布.
科学领域:
- 地质地质地质地质地质地
- 冲击石坑的形成
- 固体力学 固体力学是什么
背景情况:
- 大规模撞击会产生巨大的能量,导致岩石蒸发,融化和裂变.
- 破碎圆是具有层级条纹图案的独特地质特征,长期被认为是大物体冲击的明确指标.
- 破碎圆形成的精确机制仍然是一个未解决的科学.
研究的目的:
- 为了阐明破碎圆条纹的形成过程.
- 为了解释观察到的条纹角度与撞击地点距离之间的关系.
- 为破碎圆发展提供定量模型.
主要方法:
- 沿断裂前线进行非线性波传播的理论建模.
- 在断裂网络中对层次分叉的分析.
- 在肯特兰和弗雷德福特冲击地点进行现场测量.
主要成果:
- 破裂条纹是非线性前波沿断裂前线传播的自然结果.
- 该模型解释了条纹角随着距离撞击的距离的系统增加.
- 断裂传播速度各不相同,在雷利波速度下形成的接近撞击的圆和较远的圆在较慢的速度下形成.
结论:
- 这项研究为破碎圆形成提供了新的解释,将它们与非线性波动力学联系起来.
- 这些发现提供了对极端应力下的固体冲击动态和能量消散的见解.
- 量化预测与主要影响结构的现场数据保持一致.
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