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震中上方的位移:2011 年东北-关东地震。

Displacement above the hypocenter of the 2011 Tohoku-Oki earthquake.

机构信息

Hydrographic and Oceanographic Department, Japan Coast Guard, 5-3-1 Tsukiji, Chuo-ku, Tokyo 104-0045, Japan.

出版信息

Science. 2011 Jun 17;332(6036):1395. doi: 10.1126/science.1207401. Epub 2011 May 19.

Abstract

The moment magnitude (M(w)) = 9.0 2011 Tohoku-Oki mega-thrust earthquake occurred off the coast of northeastern Japan. Combining Global Positioning System (GPS) and acoustic data, we detected very large sea-floor movements associated with this event directly above the focal region. An area with more than 20 meters of horizontal displacement, that is, four times larger than those detected on land, stretches several tens of kilometers long along the trench; the largest amount reaches about 24 meters toward east-southeast just above the hypocenter. Furthermore, nearly 3 meters of vertical uplift occurred, contrary to observed terrestrial subsidence.

摘要

2011 年日本东北近海发生矩震级(M(w))9.0 级特大地震。我们结合全球定位系统(GPS)和声学数据,在震中上方直接检测到与该事件相关的非常大的海底运动。沿海沟延伸几十公里长的区域发生了超过 20 米的水平位移,是陆地探测到的位移的四倍;最大位移量约为 24 米,朝向震中东南方向。此外,还发生了近 3 米的垂直隆起,与观测到的地面沉降相反。

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