活断層が発生させた2007年能登半島地震津波

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タイトル別名
  • The 2007 Notohanto Earthquake Tsunami generated by an active fault
  • カツダンソウ ガ ハッセイ サセタ 2007ネン ノト ハントウ ジシン ツナミ

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説明

We carried out numerical simulations of the 2007 Notohanto Earthquake Tsunami and estimated the source based on a fault model. The basic equation is linear shallow water theory and an instantaneous generation of the tsunami was assumed based on a static fault model. In the comparison with the observation we used tide gauge records of the tsunami. The estimated fault is 25 km in length and the vertical displacement of the sea bottom is about 0.3 m in the maximum. The location coincides with an active fault formerly found in the sea bottom. As the result we concluded that the tsunami was excited by active fault.

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