2024年7号门多西诺断层地震中的光纤图像超级剪切动态
James Atterholt1, Jeffrey J McGuire2, Andrew J Barbour3
1Geologic Hazards Science Center, United States Geological Survey, Golden, CO, USA.
概括
在门多西诺断层发生了7级地震, 揭示了断层物理与复杂断层结构的相互作用. 这项技术可以改善地震预警系统.
科学领域:
- 地质学
- 地震学
- 地震科学
背景情况:
- 地震破裂的动态与断层结构密切相关.
- 密集的地震网络和新型传感技术对于高分辨率地观测地震行为至关重要.
- 光纤传感为长期,高分辨率的地震测量提供了一个有前途的方法.
研究的目的:
- 通过光纤传感研究断层结构与地震破裂物理之间的关系.
- 拍摄一个中等到大地震的破裂过程,
- 评估光纤传感对于实时地震参数估计的实用性.
主要方法:
- 在门多西诺断层附近部署密集的光纤地震阵列.
- 使用光纤阵列记录7级地震.
- 在图像破裂传播中应用地震束形成技术.
主要成果:
- 这次地震的裂以低裂速向东扩散.
- 破裂暂时停滞在结构复杂的门多西诺三合口附近.
- 破裂过渡到超级剪切速度后停滞.
- 观测了岩层异质性和地震破裂特征之间的相关性.
结论:
- 石质层的异质性对第一级地震破裂的特征有很大影响.
- 纤维光学传感为了解地震物理提供高分辨率数据.
- 这项技术有助于提升地震预警系统的实时性.
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