从洛杉矶大都会下方的地震减弱变化中发现断层和流体驱动的地震过程的证据
Chiara Nardoni1,2, Patricia Persaud3
1Department of Geology and Geophysics, Louisiana State University, Baton Rouge, LA, USA. chiara.nardoni4@unibo.it.
Scientific reports
|July 30, 2024
概括
这项研究揭示了流体驱动的过程,而不仅仅是区域压力,可能会导致洛杉矶的地震活动. 高分辨率的地震减弱模型显示了流体影响断层网络和地震演变的证据.
科学领域:
- 地质物理学 地质物理学
- 地震学 地震学
- 地球科学 地球科学 地球科学
背景情况:
- 洛杉矶地区的地震性主要与区域压力有关.
- 地震序列表明,除断层线之外的次要过程可能参与其中.
- 结合地质物理数据的地震减弱有助于确定与地震性相关的属性.
研究的目的:
- 为了创建洛杉矶市中心以东的高分辨率3D地震减弱模型.
- 调查二次过程的作用,可能是流体驱动的,在地震演变中的作用.
- 通过描述近断层区域和岩石流体性质,改进地震危险评估.
主要方法:
- 利用了来自当地地震的5600个三元地震图.
- 采用密集的地震阵列来获取数据.
- 应用了依赖频率的峰值延迟和coda减弱断层扫描.
主要成果:
- 开发了3D地震减弱模型,显示出明显的散射和吸收模式.
- 在库卡蒙加和圣哈辛托断层沿线确定了高散射灵敏度.
- 观察到一个低散射通道从圣安德烈亚斯断层向西延伸.
- 在Fontana地震序列附近检测到高吸收和低散射,表明流体参与.
结论:
- 地震减弱成像提供了对地下物质和过程的洞察.
- 有证据表明,流体驱动的机制有助于地震性和地震迁移.
- 该研究提高了对近断层区域和岩石流体相互作用的理解,以评估地震危险.
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