在日本东北部使用大规模海底和陆地网络数据进行衰减断层扫描
Yadab P Dhakal1, Ryoichi Nakamura2, Takashi Kunugi3
1National Research Institute for Earth Science and Disaster Resilience, Tsukuba, Japan. ydhakal@bosai.go.jp.
地震断层扫描显示,日本沟板边界附近有一个低衰减区域,可能是由于富含水的海洋地和沉积物. 这项研究增强了对潜水带地震危害的理解.
科学领域:
- 固体地球科学 固体地球科学
- 地震学 地震学
- 地质物理学 地质物理学
背景情况:
- 已知日本东北部的异质衰减结构.
- 由于数据限制,海上板块边界减弱的理解仍然很差.
- 2011年东北地震促使海底S-net的建立.
研究的目的:
- 为了研究日本沟潜伏区周围的三维地震减弱结构 (Qs).
- 利用来自S-net海底观测站和陆地站的数据.
- 了解海上和陆上地区的衰减变化.
主要方法:
- 从加速图中计算出S波里埃光谱.
- 应用地震断层扫描原理. 应用地震断层扫描原理.
- 利用来自150个S-net观测站和陆地站的数据.
主要成果:
- 在海上海洋板的上层表面附近确定了一个突出的低至中等的Qs区域.
- 解释这个区域为水丰富的海洋地和浮沉沉积物的标志.
- 在陆上和离岸地区观察到中度至强度的依赖频率的Qs结构.
结论:
- 该研究提供了对潜伏区衰减结构的关键见解.
- 这些发现有助于了解潜伏区的地震危险.
- 需要进一步的研究才能充分理解依赖频率的衰减行为.
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