| Œf�ÚŽGŽ��i˜a�j�F | “ú–{’n�k�HŠwƒVƒ“ƒ|ƒWƒEƒ€˜_•¶�W |
| Vol�F | 10-1Šª |
| ”N�F |
1998”N
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| •Å�F |
1159-1164•Å
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| ’˜ŽÒ�i˜a�j�F |
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| ƒ^ƒCƒgƒ‹�i˜a�j�F |
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| �´˜^�i˜a�j�F |
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| ƒL�[ƒ��[ƒh�i˜a�j�F |
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| Œf�ÚŽGŽ��i‰p�j�F |
THE EARTHQUAKE ENGINEERING SYMPOSIUM PROCEEDINGS
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| ’˜ŽÒ�i‰p�j�F |
Shigeo KINOSHITA,Makoto MIYAMOTO,Yasushi WADA,Yousuke OGUE,Akira NARITA,Masayoshi UEHARA,Aketo SUZUKI
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| ƒ^ƒCƒgƒ‹�i‰p�j�F |
K-NET
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| �´˜^�i‰p�j�F |
From the Kobe Earthquake 1995, we learned that more information on strong-motion in a hypocenter area is necessary to investigate the generation of strong-quake and to assess the degree of disaster for quick mitigation responses. The K-NET, a 1,000-elements strong-motion network, was deployed in 1996 for responding these requests. After about one year, the K-NET transmitted one million data files to users on the Internet. This means that the K-NET is well responding to user requests. In this article, we explain the K-NET.
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ˆÏˆõ‰ï˜_•¶�W |