On the basis of the field investigation and geological interpretation of seismic  profiles of Jiamusi uplift and surrounding Mesozoic-Cenozoic basins in Northeast China, combined with recent research results, the basin-mountain coupling are determined. The uplifting of Jiamusi uplift in Mesozoic-Cenozoic is mainly the results of twice thrusting superposition in Late Cretaceous and Oligocene-Miocene. The study area has always been active continental margin tectonic setting since the Cretaceous, the above three stages of basin-mountain coupling are related with the subduction of the Pacific Plate to the Eurasian plate.