| 1. | After that , features of antiplane surface motion for several typical sites are studied in details by use of superiority of analytical solutions in probing into objective regularity
然后，利用解析解探讨客观规律方面的优势，对几种典型场地出平面地表运动特征做了详细的研究。 |
| 2. | ( 3 ) comparison analysis for antiplane surface motion features between the circular - arc cross - section alluvial valley and the single overburden layer is investigated in details in this paper
( 3 )为了更深入地研究了一般圆弧状沉积盆地的出平面地表运动特征，本文与已有的软土单覆盖层解析结果做了对比分析。 |
| 3. | In the fabrication of diffractive optics elements and semiconductor , it is demonstrated that an initial edger can expand into smooth curves and the surface motion in different local place is not identical
在制作衍射光学元件以及半导体加工的刻蚀工艺中，刻蚀产生的表面面形随刻蚀时间的延长而产生动态的形变。 |
| 4. | The notable torsion effects of the surface ground motion above the alluvial valley are illustrated and the torsion effects become stronger as the frequency of the incidence is higher . ( 4 ) antiplane surface motion of the underground circular soft inclusion and the underground homogeneous soft interlayer is investigated in this paper . the results indicate : surface displacement amplitudes just above the soft inclusion of small depth - to - width ratio is amplified and soft interlayer of small depth - to - thickness ratio is amplified to a certain degree , and moreover , the latter is lower limit of the former
结果表明：垂直入射时，小深宽比软夹塞上方地表位移幅值有较大的放大，小深厚比软夹层的地表位移幅值也有一定的放大，且后者为前者的下限；波接近掠入射时，软夹塞正上方地表点和软夹层的中国地震局工程力学研究所硕士学位论文一地表位移幅值都没有放大，而软夹塞迎波面一侧地表点的位移幅值会有一定的放大；软夹塞上方的地表位移运动有较强烈的扭转效应，且此扭转效应随入射波频率的增高而增强。 |
| 5. | ( 5 ) antiplane surface motion of underground circular hard inclusion and underground homogeneous hard interlayer is investigated . the results indicate : the surface displacement amplitudes just above the underground circular hard inclusion is reduced , while surface motion on both two sides are significantly amplified when the vertical waves are excited . the surface motion on the side o
结果表明：波垂直入射时硬夹塞上方地表位移幅值处于减小状态，但在两侧出现放大，波斜入射时硬夹塞的迎波一侧地表易出现一定的放大：硬夹层上的地表位移幅值在多数情况下呈现一种放大作用，对深厚比较大的硬夹层放大作用易出现在低频：地下硬夹塞上的地表运动没有明显的扭转效应。 |
| 6. | After that , antiplane surface motion features of the shallow alluvial valley of small depth - to - width ratio are investigated in details . the results indicate that surface displacement amplitudes of alluvial valley will not reduce when the alluvial valley become shallow . the maximum amplitudes will move to high frequency with depth - to - width ratio becoming small
在此基础上，对小深宽比的浅圆弧型沉积盆地出平面地表运动特征做了较深入的研究，结果表明盆地地表位移幅值不会因变浅而减小，最大反应会随着盆地深宽比的减小而向高频移动。 |
