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1966 Hualien earthquake : ウィキペディア英語版 | 1966 Hualien earthquake
The 1966 Hualien earthquake occurred on March 13 at .〔http://tao.cgu.org.tw/pdf/v93p487.pdf〕 The epicenter was located in the offshore area between Yonaguni Island, Japan and Hualien, Taiwan. The intensity in Yonaguni reached shindo 5. 2 people were reported dead in Yonaguni, Japan, and 4 in Taiwan. Building damage was reported. A tsunami with a run-up height of was observed. This earthquake released a seismic moment of 4.86×1020 Nm. The magnitude of this earthquake was put at Ms 8.0, Mw7.79,〔http://ntur.lib.ntu.edu.tw/bitstream/246246/173952/1/32.pdf〕 Mjma 7.8, or ML 7.8.〔http://2007tga.cgu.org.tw/cdrom/Oral%20(PDF)/O4-3A-04.pdf〕 This earthquake had a strike-slip faulting focal mechanism. The fault plane solutions of this earthquake suggested that there is a sliver of crust off the east coast of Taiwan other than the Philippine Sea Plate. The map of shallow earthquakes shows that the Philippines are encircled by a zone of seismicity. There is a difference between the slip direction in the east coast of the Philippines and the relative motion between the Philippine Sea Plate and the Eurasian Plate. Together with other evidences, it has been suggested that most of the Philippines might belong to a minor plate other than the Eurasian Plate.〔http://www.eri.u-tokyo.ac.jp/seno/Papers/tecphys1977.phs.pdf〕 == References ==
抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)』 ■ウィキペディアで「1966 Hualien earthquake」の詳細全文を読む
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