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在2025年MW7.7的缅甸地震期间,异质的破裂和屏障机制
Şule Gürboğa1, Fatma Canaslan Çomut2, Sen Lyu3,4
1Faculty of Mines, Department of Geological Engineering, İstanbul Technical University, İstanbul, Türkiye. sulegurboga@itu.edu.tr.
2025年缅甸地震在萨断层造成了显著的表面破裂,地面的移位高达4.5米. 断层结构和岩石特性影响了地震的发生.
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
- 遥感 遥感 遥感 遥感
背景情况:
- 2025年缅甸7.7级地震发生在萨断层,这是一个主要的转变断层.
- 随后在曼德拉附近发生了6.7级的地震.
研究的目的:
- 通过实地调查和卫星"卫星"号SAR图像分析表面断层偏移.
- 为了了解控制共地震滑动分布的因素.
主要方法:
- 补偿 追踪分析卫星Sentinel-1SAR卫星图像.
- 实地调查以测量地面移位.
主要成果:
- 在萨断层沿线观察到超过3米的地面位移.
- 在曼德拉附近,局部偏移达到4-5米.
- 在Naypyidaw附近测量了4.5米的最大位移.
结论:
- 断层偏移分布受 rheological 变化和地下岩石效应的影响.
- 不同质的风湿学和细分断裂导致了不均的滑动分布.
- 以前存在的断层结构显著控制了共地震滑动模式.
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