在2011年东北奥基地震的低中心上方的位移
Mariko Sato1, Tadashi Ishikawa, Naoto Ujihara
1Hydrographic and Oceanographic Department, Japan Coast Guard, 5-3-1 Tsukiji, Chuo-ku, Tokyo 104-0045, Japan. eisei@jodc.go.jp
概括
2011年东北奥基地震造成了海底巨大的移动,水平移动超过20米,在震中附近出现了显著的垂直升起. 这些发现揭示了巨大的推力事件期间前所未有的海底地质变化.
科学领域:
- 地质物理学 地质物理学
- 地震学 地震学
- 海洋学 海洋学 海洋学
背景情况:
- 2011年东北奥基地震是一个9.0级的巨大推力事件,发生在日本海岸附近.
- 了解海底变形对于地震危险评估至关重要.
研究的目的:
- 为量化与2011年东北奥基地震相关的海底移位.
- 将海底运动与陆地观测进行比较.
主要方法:
- 全球定位系统 (GPS) 和声学数据的综合分析.
- 在地震的焦点区域内直接检测海底运动.
主要成果:
- 检测到广泛的水平海底移动超过20米,明显大于陆地移动.
- 测量到的最大水平移位大约为24米,向东-东南方向.
- 观察到近3米的垂直海底升起,与沿海沉降形成鲜明对比.
结论:
- 2011年东北奥基地震产生了非常大的海底移位.
- 海底变形模式与在陆地上观察到的差异很大.
相关概念视频
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To describe the motion of an object, one should first be able to describe its position (where it is at any particular time). More precisely, the position needs to be specified relative to a convenient frame of reference. A frame of reference is an arbitrary set of axes from which the position and motion of an object are described. Earth is often used as a frame of reference to describe the position of an object in relation to stationary objects on Earth.
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