Abstract Using drilling and shear wave velocity logging data collected from 43 engineering sites of seismic safety evaluation projects completed in Changzhi urban district, the structural models of shallow strata and shear wave velocity are built in terms of the Kriging interpolation, which is an unbiased evaluation method for non-uniform distribution of discrete data. The results show that the shallow strata and shear wave velocity structures present stronger laterally inhomogeneous features, and also indicate that the sedimentary deformation is obviously controlled by the hydrological environment as well as the main faults in Changzhi urban district and its adjacent areas.
GENG Wei,XU Zhaofan,LIU Yan et al. The Structural Characteristics of Shallow Strata and Shear Wave
Velocity in Changzhi Urban District[J]. jgg, 2015, 35(5): 840-843.
GENG Wei,XU Zhaofan,LIU Yan et al. The Structural Characteristics of Shallow Strata and Shear Wave
Velocity in Changzhi Urban District[J]. jgg, 2015, 35(5): 840-843.
