概括
南加州正在经历显著的地升起,测量0.15到0.25米,始于1960年左右. 这个地质事件覆盖了超过12,000平方公里,以圣安德烈亚斯和加洛克断层附近为中心.
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
- 地质测量是指地质测量.
背景情况:
- 南加州呈现着持续的地变形和移动性.
- 历史上的地质测量数据揭示了该地区构造活动的模式.
研究的目的:
- 分析和报告南加利福尼亚州一个显著的地升起事件.
- 为了划出这个升起的空间范围和时间演变.
主要方法:
- 历史地质记录的分析.
- 对跨越几十年的地变形数据的检查.
主要成果:
- 已经确定了0.150.25米的地升起,从1960年左右开始.
- 升起影响至少12,000平方公里,沿着圣安德烈亚斯断层延伸到横跨山脉和莫哈韦区块.
- 这一事件似乎从圣安德烈亚斯断层和加洛克断层交汇处附近的中心发作了.
结论:
- 观察到的升起是一个大而潜在的独特事件,叠加在现有的变形模式上.
- 这次升起发生在一个自1932年以来基本上无地震的地区,突出显示了不寻常的构造活动.
- 持续监测对于了解这种显著地变形的影响至关重要.
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