| 一种地壳垂直形变新模型 |
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| 引用本文： | 刘权威 孙国学. 一种地壳垂直形变新模型[J]. 山西地震, 1994, 0(1): 12-17 |
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| 作者姓名： | 刘权威 孙国学 |
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| 作者单位： | 太原工业大学，山西省地震局 |
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| 摘 要： | 研究了建立整个形变区域的形变速率曲面和形变加速率曲面，以及求这两种曲面的方法（基于多元逐步回归分析的间接法和直接法），建立了一个对整个形变区域形变的整体概念，据此，可得出形变区任何一个已知其平面位置的点在任一观测期内的形变量。
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| 关 键 词： | 动态平差，速率曲面，加速率曲面 |
A New Model of Crustal Vertical Deformation |
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| Liu Quanwei. A New Model of Crustal Vertical Deformation[J]. Earthquake Research in Shanxi, 1994, 0(1): 12-17 |
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| Authors: | Liu Quanwei |
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| Affiliation: | Liu Quanwei(Industry Univercity of Taiyuan)sun Guoxue(Seismological Bureau of Shanxi Province ) |
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| Abstract: | Based on the indirect and direct methods of multiple stepwise regression,the establishment of the curvedsurface ofdefOrmation rate and acceleration in whole deformation area has been studied.A complete conceptof the deformation in whole deformatica area has been constructed,so that the deformation quantity of anypoint in the deformation area during any observation can obtained. |
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| Keywords: | dynamic adjustment curved surface of rate cueved surface of acceleration |
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