Abstract:In 1985, we calculated the travel-time table of regional seismic waves by using a two-layer crustal model, H1=22.0km, Vp1=6.10km/—sec, Vs1=3.55km/sec; H2=29.5km, Vp2=6.47km/sec, Vs2=3.81km/sec; H=51.5km, Vpn= 8.17km/sec, Vsn=4.62km/sec. Besides giving the travel times ofp,s, P2, S2, Pn, Sn waves with the general travel-time table, it also gave the travel times of P1, S1 reflection waves at the surface of the middel layer and of Pm, Sm reflection waves at the Moho surface. This table is more practical than that calculated by a one-layer model of Gansu and its adjacent areas, and more accurate than that calculated by a four-layer location model of Gansu area. It is used conveniently.