**6. Conclusion**

All the suggested geodynamic reconstructions of the studied region take into account the interdependence between North-Asian and China-Korea plates and plates of the Pacific basin oceanic crust [16]. The suggested work attempts to show the dependence of the evolution of the Bureya-Jiamusi superterrane on the surrounding geological objects in the late Cretaceous-Cenozoic interval. As a result of the analysis of the original and extensive literature, it is suggested that magmatic activity—its manifestations and activity changes—in the Bureya-Jiamusi superterrane territory correlates quite well with the geodynamic events occurring in the late Mesozoic-Cenozoic, not only on the continental margin of Asia but also within the evolution of oceanic plates of the Pacific basin (plate Izanagi). Comparison of the time stages, material composition, and tectonic positions of the Bureya-Jiamusi superterrane in this time interval indicates its belonging to the structures of the Pacific mobile belt.
