概括
在加利福尼亚州帕克菲尔德附近检测到的断层区域头波显示,圣安德烈亚斯断层的速度对比度为4%. 这些地震波为断层系统变化提供了洞察力.
科学领域:
- 地震学 地震学
- 地震科学 地震科学 地震科学
- 地质物理学 地质物理学
背景情况:
- 由加利福尼亚州帕克菲尔德附近的一个钻井地震网络记录的微型地震地震图.
- 分析侧重于圣安德烈亚斯断层沿线地震事件的第一个P波到来.
研究的目的:
- 为了识别和描述沿圣安德烈亚斯断层折射的地震头波.
- 使用这些波来推断断裂区物质对比的特性.
主要方法:
- 分析新兴到达和直接P波之间的旅行时间差异.
- 检查波形特征 (涌现与尖的第一次断裂).
- 首次运动极性与断层区域头波理论预测的比较.
主要成果:
- 三条证据证实了第一个P的到来是头波.
- 旅行时间差异与距离线性扩大.
- 新兴波特征和逆极性与头波理论相匹配.
- 显示在断层中大约有4%的速度对比.
结论:
- 断层区域头波存在于当地地震网络数据中.
- 这些波可以解释地震地点的分散和源机制.
- 头波提供了一种评估故障系统物理状态变化的方法.
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