A laboratory study of teleseismic Pn waves

Abstract

In this paper, the influences of mechanical properties of low velocity layers and thickness of high velocity layers in the lower lithosphere on the horizontal propagaties of seismic waves are discussed by means of altrasonic seismic model experiments; It is shown that the structure of the lower lithosphere consisting of soft low velocity layers and thin high velocity layers is favourable for the horizontal propagation of seismic energy, therefore, it is a very possible structure pattern of the lower lithosphere responsible for Pn and later high velocity arrivals observed in long range distances; Such pattern is also consistent with studies of rheological stratification of the lower lithosphere beneath mid-ocean-ridges and continental rifts.