卡斯卡迪亚震位于板块接口附近,受到S减去P波倍的约束
Mario La Rocca1, Kenneth C Creager, Danilo Galluzzo
1Istituto Nazionale di Geofisica e Vulcanologia-Osservatorio Vesuviano, Via Diocleziano 328, 80124 Napoli, Italy. mlarocca@ov.ingv.it
概括
确定非火山震动的位置是一项挑战. 这项研究使用地震波 (S和P波) 时间延迟来确定震源深度,揭示它们起源于引板附近.
科学领域:
- 地震学 地震学
- 地震研究 地震研究
- 构造学 构造学 构造学 构造学
背景情况:
- 非火山震缺乏明显的地震阶段,这使得源头的定位变得复杂.
- 由于信号特征,传统的地震网络很难确定震动的起源.
研究的目的:
- 开发和应用一种用于准确定位非火山震源的新方法.
- 确定震源与构造结构的精确深度和关系.
主要方法:
- 纵向和水平地震图的交叉相关性,以识别共同的信号.
- 测量地震剪波 (S波) 和压缩波 (P波) 之间的时间滞后.
- 将S-P时间间隔与定位技术集成在一起,以解决源深度.
主要成果:
- S-P波的时间间隔准确地表示P波和S波到达之间的时间.
- 震源深度在+/-2公里内得到解决.
- 最近的卡斯卡迪亚震源位于或靠近潜水板接口.
结论:
- 该S-P波延迟方法有效地解决震源深度.
- 加斯卡迪亚震源于潜水板接口附近的重复来源.
- 这种技术增强了我们对潜伏区震过程的理解.
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