面波反演技术与青海地区上地壳结构

THE INVERSION OF SEISMIC SURFACE WAVE DISPERSION AND THE STRUCTURE OF UPPEK CRUST IN QINHAI AREA

摘要:

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。

Abstract:

The inversion of seismic surface wave dispersion is one of the important methods for exploring the structure of the earth's interior,in this paper,problems on inversion calculation are discussed in detail and the upper crustal structure of Qinghai area is inversed by using the information of Gansu Seismic network.