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The distinct extending gravitational lineament crosses in NNE direction the significant part of the continent from the Bacbo Bay to the Okhotsk Sea coast with changing of above mentioned negative values by more positive in the east. The distinct extending gravitational lineament crosses in NNE direction the significant part of the continent from the Bacbo Bay to the Okhotsk Sea coast with changing of above mentioned negative values by more positive in the east.

This change is connected with the sharp decreasing of the continental crust thickness. This change is connected with the sharp decreasing of the continental crust thickness. "Block Structure and Kinematics of Eastern and Central Asia from GPS Data." Geotectonic 39.5 (2005): 333 — 348.

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At the same time model vectors of horizontal displacement form a characteristic divergence with a west deflection (10° NE — 350° NW) near the west syntax of the Himalayas in NW Tibet and Tienshan and east deflection up to 50—70° NE and more near the east syntax in SE Tibet, Qaidam and in the west of the Sichuan Province of China.

The direction of the P and S -waves anisotropy shows within the great part of the region the coupling deformation in the lithosphere upper mantle and crust. The direction of the P- and S-waves anisotropy shows within the great part of the region the coupling deformation in the lithosphere upper mantle and crust. They limit blocks joined to Eurasia (before that to Laurasia) from the late Precambrian to Cenozoic.

Differently directed vectors of horizontal displacement are established in the crust and upper mantle only east of the east Himalayan syntax indicating decoupling these layers under the influence of the Hindustan-Asia collision and “a threshold” of the SE China thick lithosphere in its boundary with Tibet. Differently directed vectors of horizontal displacement are established in the crust and upper mantle only east of the east Himalayan syntax indicating decoupling these layers under the influence of the Hin-dustan-Asia collision and "a threshold" of the SE China thick lithosphere in its boundary with Tibet. Boundaries of blocks are formed now as a rule by active faults. Up-to-date block structure of central Asia and adjacent territories.

So the east boundary of the Amurian Block (Amurian Plate in other interpretation) is drawn in this work along the active Tanlu Fault and its contuniation in the Russia territory (Figure 1).

At the same time some geologists suppose, that it passes more east along the Sakhalin Fault and a segment of the Japanese subduction zone [Ashurkov et al. But in such case the east part of the south boundary of this structure will cross nearly perpendicularly NNE active faults in the east China Sea and Korean Peninsula.

In the field of up-to-date tectonic stress the compression distinctly predominates in this transit zone and changes partly on extension and slipping with extension in the east Asian zone. In the field of up-to-date tectonic stress the compression distinctly predominates in this transit zone and changes partly on extension and slipping with extension in the east Asian zone.

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