Abstract:Partial melt models in different geometrical configuration and distribution are established.The geometrical distribution and the connectiveness of the melt are determined by three factors:① the location of melt;② the melt fraction;③the minimum total free energy of the solid-solid and the solid-liquid interfaces.The melt geometries are films,tubes and isolated ellipsoidal inclusions.The bulk and shear moduli and conductivity in partially melted rocks are calculated by using the models.The vp,vs and ρ are calculated by choosing parameters in the lower crust on both sides of the northern segment of North-South seismic zone,i.e.,in the lower crust of Ordos platform vp≈ 6.71 km/s,vs≈ 3.96 km/s,resistivities are from one hundred Ωm to several hundreds Ωm,in the fold systems of Qilian and Qinling 6.4 km/s ≤vp ≤ 6.6 km/s,3.72 km/s ≤vs ≤ 3.89 km/s,resistivities are from several Ωm to dozens Ωm.The results of numerical modelling agree with that of geophysical inversion for the most part,the geotectonics are explained qualitatively.The combined numerical modelling of velocity and resistivity in lower crust by using a model shows that the model is available in interpretation of vp,vs and ρ.