The Maqen-Jingbian wide-angle seismic reflection and refraction experiment was carried out in 1998,which aims at determining detailed structure in the crust and top of the upper mantle and understanding structural relation between the northeastern Tibetan plateau and the Ordos block. The 1-D crustal models inferred by waveform inversion show strong variations in crustal structure,which can be classified into four different types:1 an Ordos platform with the Proterozoic crust and two high-velocity layers in the northeast section,2 a transitional crust between the northeastern Tibetan plateau and the Ordos block across the Haiyuan earthquake zone,3 the Qilian orogenic zone in the central part,and 4 the Qinling orogenic zone in the southwestern section. The Moho depth increases from ～42 km to ～62 km from the NE part to the SW part of the profile. The crystalline crust consists of the upper crust and lower crust in northeastern Tibetan plateau. There is an obviously low P-wave velocity layer dipping northeastward,which is 12-13 km thick,at the bottom of the upper crust in Qinling orogenic zone and Haiyuan earthquake zone. The lower crust is characterized by alternating high and low P-wave velocity layers. Beneath Ordos block,i.e.,the NE part of the profile,the crust shows quite a smooth increase in P-wave ve-locity down to the Moho at a depth of about 42 km. The Maqen-Jingbian wide-angle seismic reflection and refraction experiment was carried out in 1998, which aims in determining detailed structure in the crust and top of the upper mantle and understanding structural relation between the northeastern Tibetan plateau and the Ordos block. The 1- D crustal models inferred by waveform inversion show strong variations in crustal structure, which can be classified into four different types: 1 an Ordos platform with the Proterozoic crust and two high-velocity layers in the northeast section, 2 a transitional crust between the northeastern Tibetan plateau and the Ordos block across the Haiyuan earthquake zone, 3 the Qilian orogenic zone in the central part, and 4 the Qinling orogenic zone in the southwestern section. The Moho depth increases from ~ 42 km to ~ 62 km from the NE part to the SW part of the profile. The crystalline crust consists of the upper crust and lower crust in northeastern Tibetan plateau. There is an obvious low P-wave velocity layer dipping northeastward, which is 12-13 km thick, at the bottom of the upper crust in Qinling orogenic zone and Haiyuan earthquake zone. The lower crust is characterized by alternating high and low P-wave velocity layers. Beneath Ordos block, ie, the NE part of the profile, the crust shows quite a smooth increase in P-wave ve-locity down to the Moho at a depth of about 42 km.