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本文导出了一种给出相对烈度在lg R~0之间的收敛解(忽略震级)的小震方程式。结合在贝加尔地区岩石抗震特性调查与文字资料和统一理论,使人们可对震源等势面进行评估。确定了在震源区边界处的地震烈度稳定性和弹性波在地壳中的传播,使得推导出从地震主要参数震级向随震中距不同的烈度定量计算的转换成为可能。获得了烈度(能通量的密度)对距离的双线性相关,给出了能通量密度和相对烈度之间的关系。求出了取决于地表建筑地基的物理特性的振动载荷烈度。在地震学角度,这种强震的定量预测方法是一种提供详细地震区划和场地小区划的可能手段之一。
In this paper, we derive a small earthquake equation that gives the convergent solution (ignoring the magnitude) of the relative intensity between lg and R ~ 0. Combined with the investigation of seismic characteristics of rocks in the Baikal region and the textual data and the unified theory, people can assess the equipotential surface of the source. The stability of seismic intensity and the propagation of elastic wave in the crust at the boundary of the source region are confirmed, which makes it possible to derive the transition from the magnitude of seismic principal parameter to the magnitude of seismic intensity different from the epicenter. The bilinear correlation of the intensity (flux density) to the distance was obtained, and the relationship between flux density and relative intensity was given. The vibration load intensity which depends on the physical characteristics of the ground surface of the foundation is obtained. Seismologically, this quantitative prediction of strong earthquakes is one of the possible means of providing detailed seismic zoning and site zoning.