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一、引言 本文是专门讨论地壳板块内部某处发生地震而引起板块的垂直振动问题,这时作为板块边界的断层,或受到约束不产生位移及转角,或者震中距边界太远而几乎没有波及到边界上,这样我们就可以把板块的边界当作固定边。此外本文提供的方法,还可适用于板块内部在长期高温高压下产生的静力垂直变形问题。这里是用弹(塑)性薄板(壳)的理论来解决地球力学问题。我们看到特可忒(Turcotte)等三人在1976年8月于澳大利亚
I. INTRODUCTION This article is devoted to the issue of vertical vibration caused by earthquakes somewhere in the crustal plate. At this moment, the faults that are the boundaries of the plate are restrained without displacement and rotation or the epicenter is too far away from the boundary to reach Boundary, so that we can use the plate boundary as a fixed edge. In addition, the method provided in this paper can also be applied to the problem of static vertical deformation caused by long-term high temperature and pressure inside the slab. Here is the theory of shells (plastic) sheet (shell) to solve the problem of geomechanics. We saw three people such as Turcotte in Australia in August 1976