摘要
The magnetotelluric exploration profile of Maqu-Beichuan shows the extent and structure characters of upper crust,lower crust and upper mantle along the sections.First,there exists a large nappe structure from north China block to Longmenshan tectonic belt between the overlying strata of upper crust and basement.Second,the thickness of upper crust,especially the one of crystalline basement,limits the stability of blocks.Third,the relief of low-resistivity layer in the crust and the swell or sag of Moho are close correlative to the stability of blocks.