人类调节和蒸发物溶解对地震引发的地面故障的影响
Paula Bürgi1, Eric M Thompson2, Kate E Allstadt2
1U.S. Geological Survey Geologic Hazards Science Center, Golden, CO, USA. pburgi@usgs.gov.
Nature communications
|March 8, 2024
概括
在里奇克雷斯特地震之后,西尔尔斯湖的六角表面喷射并不是由液化引起的. 相反,溶解腔崩 (DCC) 被提出为可能的机制,挑战现有的地震触发的地面故障模型.
科学领域:
- 地质物理学 地质物理学
- 遥感 遥感 遥感 遥感
- 地震工程的工程是地震工程.
背景情况:
- 2019年里奇克雷斯特地震导致西尔尔斯湖的地面变形和表面喷射.
- 以前的研究经常将这种现象归因于土壤液化.
- 在溶液采矿操作附近观察到表面喷射的独特六角形图案.
研究的目的:
- 为了调查在西尔尔斯湖观察到的六角形表面喷射的原因.
- 评估溶解腔塌 (DCC) 作为液化替代机制的作用.
- 评估非液化地面故障机制对地震危险模型的影响.
主要方法:
- 分析遥感数据,包括交叉测量合成孔径雷达 (InSAR),以检测地面变形.
- 检查与西尔尔斯湖地区和采矿业务相关的地质和地质技术数据.
- 观察到的地面故障模式与液化和溶解腔崩模型的预测进行比较.
主要成果:
- 六角形的表面喷射模式与经典的液化不一致.
- 事件发生前的InSAR数据显示了差异性沉降和地下空洞形成,支持DCC.
- 溶解腔塌 (DCC) 可能在低于液化的地震震动值时触发.
结论:
- 溶解腔塌 (DCC) 被提出为观察到的六角表面喷射的主要机制.
- 非液化地面故障机制可能被误认为是液化,在预测模型中引入偏差.
- 遥感对于识别和解开地震触发的复杂地面故障过程是有价值的.
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