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| ＳＴＵＤＹＯＮＳＥＩＳＭＯＴＥＣＴＯＮＩＣＤＹＮＡＭＩＣＳＯＦＱＩＮＧＨＡＩＴＩＢＥＴ ＰＬＡＴＥＡＵＦＲＯＭ ＩＳＯＳＴＡＴＩＣＧＲＡＶＩＴＹＡＮＯＭＡＬＩＥＳ |
| ＸｉｎｇＬｅｌｉｎ １，２，３;ＬｉＪｉａｎｃｈｅｎｇ３;ＬｉＨｕｉ １，２;ＺｏｕＺｈｅｎｇｂｏ １，２;ＺｈｏｕＸｉｎ １，２ |
| １）ＩｎｓｔｉｔｕｔｅｏｆＳｅｉｓｍｏｌｏｇｙ，ＣＥＡ，Ｗｕｈａｎ ４３００７１ ２）ＣｒｕｓｔａｌＭｏｖｅｍｅｎｔＬａｂｏｒａｔｏｒｙ，Ｗｕｈａｎ ４３００７１ ３）ＳｃｈｏｏｌｏｆＧｅｏｄｅｓｙａｎｄＧｅｏｍａｔｉｃｓｏｆＷｕｈａｎＵｎｉｖｅｒｓｔｉｙ，Ｗｕｈａｎ ４３００７９ |
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Abstract ＯｎｔｈｅｂａｓｉｓｏｆｔｈｅＡｉｒｙＨｅｓｉｋａｎｎｅｎｅｑｕｉｌｉｂｒｉｕｍｈｙｐｏｔｈｅｓｉｓ，ｔｈｅｉｓｏｓｔａｔｉｃｇｒａｖｉｔｙａｎｏｍａｌｉｅｓｏｆＱｉｎｇ ｈａｉＴｉｂｅｔｐｌａｔｅａｕａｒｅｃａｌｃｕｌａｔｅｄｔａｋｉｎｇｔｈｅｄｅｎｓｉｔｙａｎｄｔｈｅｄｅｐｔｈｏｆｕｐｐｅｒｌｉｔｈｏｓｐｈｅｒｅｆｒｏｍｔｈｅＣＲＵＳＴ２．０ｍｏｄｅｌａｓ ｐａｒａｍｅｔｅｒｓ，ａｎｄｔｈｅｎｔｈｅｓｅｉｓｍｏｔｅｃｔｏｎｉｃｄｙｎａｍｉｃｓｉｓｓｔｕｄｉｅｄｂｙｕｓｅｏｆｔｈｅｓｅｉｓｍｉｃｄａｔａｆｒｏｍｔｈｅｐｏｉｎｔｏｆｅｑｕｉｌｉｂｒｉｕｍ．Ｉｔｓｈｏｗｓｔｈａｔｓｔｒｏｎｇｅａｒｔｈｑｕａｋｅｓｏｃｃｕｒｏｆｔｅｎｉｎｔｈｅｉｎｆｌｅｘｉｏｎｏｆｇｒａｄｉｅｎｔｂｅｌｔｏｆｉｓｏｓｔａｔｉｃｇｒａｖｉｔｙａｎｏｍａｌｉｅｓ，ａｎｄ ｇｅｎｅｒａｌｌｙ，ｔｈｅｏｃｃｕｒｒｅｎｃｅｏｆｅａｒｔｈｑｕａｋｅｉｓｃｏｒｒｅｌａｔｅｄｔｏｃｒｕｓｔｔｅｃｔｏｎｉｃ
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| Key words：
ｅａｒｔｈｑｕａｋｅ
ＱｉｎｇｈａｉＴｉｂｅｔｐｌａｔｅａｕ
ｉｓｏｓｔａｔｉｃｇｒａｖｉｔｙａｎｏｍａｌｙ
ＣＲＵＳＴ２．０ｍｏｄｅｌ
ｔｅｃｔｏｎｉｃｍｏｖｅｍｅｎｔ
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Received: 01 January 1900
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Corresponding Authors:
ＸｉｎｇＬｅｌｉ
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| Cite this article: |
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ＸｉｎｇＬｅｌｉｎ,ＬｉＪｉａｎｃｈｅｎｇ,ＬｉＨｕｉ et al. ＳＴＵＤＹＯＮＳＥＩＳＭＯＴＥＣＴＯＮＩＣＤＹＮＡＭＩＣＳＯＦＱＩＮＧＨＡＩＴＩＢＥＴ ＰＬＡＴＥＡＵＦＲＯＭ ＩＳＯＳＴＡＴＩＣＧＲＡＶＩＴＹＡＮＯＭＡＬＩＥＳ[J]. , 2007, 27(6): 33-36.
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ＸｉｎｇＬｅｌｉｎ,ＬｉＪｉａｎｃｈｅｎｇ,ＬｉＨｕｉ et al. ＳＴＵＤＹＯＮＳＥＩＳＭＯＴＥＣＴＯＮＩＣＤＹＮＡＭＩＣＳＯＦＱＩＮＧＨＡＩＴＩＢＥＴ ＰＬＡＴＥＡＵＦＲＯＭ ＩＳＯＳＴＡＴＩＣＧＲＡＶＩＴＹＡＮＯＭＡＬＩＥＳ[J]. jgg, 2007, 27(6): 33-36.
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| URL: |
| http://www.jgg09.com/EN/ OR http://www.jgg09.com/EN/Y2007/V27/I6/33 |
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