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利用地震面波频散反演,是探测地球内部结构的重要手段之一。本文详细地讨论了面波频散反演计算中的具体问题,并利用甘肃台网资料反演出青海地区上地壳模型。
Using seismic surface wave dispersion inversion is one of the important means to detect the internal structure of Earth. This paper discusses in detail the specific problems in the calculation of surface wave dispersion inversion and the inversion of the upper crustal model in Qinghai by using the Gansu network data.