**1. Introduction**

In 2013–2018, authors analyzed at the relatively small scale the structure and seismicity of intracontinental interblock zones within the Asiatic part of Russia and adjacent countries together with calculation of the releasing seismic energy and construction of their dissipation graphs as well as the deep seismic sections [1, 2]. The results of this analyzing allowed selecting the most active seismic zones, including overwhelming majority of minor and strong earthquakes' epicenters, and examined in detail the lithosphere deep structure under them and not far of them with establishing the possible connection of these zones with the geodynamic activity and anomalies of different geophysical fields. With special attention, we considered kinematics of blocks and main lithosphere plates as well as the connection with them active processes in interblock zones. All blocks considered in our paper are delineated by active

faults, data on which we taken from the works of [3, 4], including results of author's field investigations in Transbaikalia in 2008 [5]. The modern block structure of central Asia was considered and validated in some previous author's works [1, 6–8].

In 2018–2020, we investigated in the more large scale the influence of the deep and near surface lithosphere structure on the interblock zones geodynamic activity with possible levels of seismic energy releasing. Within the most active from these zones, we established areas with seismic energy maximal releasing. They situate in the northwest Altai together with the adjacent part of the west Sayany, in the west of the east Sayany, around the Baikal Lake and in northwest Transbaikalia, in the east of Transbaikalia between the Vitim River and upper stream of the Aldan River and in the north of the Sakhalin Island.
