Том 12, № 4 (2018)

Geodynamic and seismic activation in the southeastern part of Far Eastern Russia is associated with nucleation of strain waves in the buffer zone of the Amurian Plate when it moves northeastward. The highest crustal seismicity is typical of Lower Priamurye, where a zone of М ≥ 4.5 earthquakes originated in its central part that was related to reactivation of the Bureya Orogen. The maximum of the regional compression is confined to the meridional dome, under which the depth of the Moho discontinuity increases from 36 to 40 km. The area of lower rock density in the central part of the Bureya Orogen is exhibited by an intense negative gravity anomaly. A contemporary uplift of the orogen initiated the centrifugal migration of seismicity during 1983–2009, when epicenters of М ≥ 5.0 earthquakes migrated from the center of the dome to its periphery. Strong earthquakes (М ≥ 5.0) are also concentrated south of the Bureya Orogen in the transregional Tan-Lu Fault zone, where the earthquake foci migrate in the northeastern direction. Geodynamic activation is controlled here by the tangential rotation (pressure) of the Amurian Plate, forcing the Central Sikhote-Alin tectonic block to move in the southern direction. North of the block, a 500 × 950 km crustal plate is formed due to extension, which is inclined along the Tan-Lu Fault. In the compression area, a mountain uplift of the same name is formed at the opposite boundary of the Central Sikhote-Alin block. Being rotated clockwise, the block interacts with the subduction zone of the Pacific Plate at a depth of 400–600 km, where deep-focus earthquakes with М ≥ 6.0 are generated due to bilateral pressure.

It is established that the igneous rocks of the northern Bureya continental massif, which are ascribed to the Amur, Drevnyaya Bureya, and Nyatygran complexes, are Late Paleozoic and Early Mesozoic in age, not early Precambrian as previously assumed. The ages obtained correspond to two stages of magmatic activity: ~264 and ~194 Ma. These stages are clearly manifested in the other continental massifs of the Central Asian Fold Belt, which suggest the common tectonic origin of the magmatic activity. All of the studied igneous rocks ascribed to the Amur, Drevnyaya Bureya, and Nyatygran complexes, despite their Late Paleozoic and Mesozoic ages, bear traces of structural–metamorphic transformations.

The deposits of the Imlekin Formation of the Upper Pegtymel depression were formed in the southern margin of the Chukotka Terrane synchronously with accretion of the Kulpolney island arc to the Chukotka–Arctic Alaska microplate. The sedimentological structural features of the Upper Jurassic–Lower Cretaceous sections indicate their accumulation within various parts of submarine fans of a shallow marine basin. The submarine slump origin of the boulder–pebble (tillite-like) conglomerates is substantiated. The petrographic, geochemical, and geochronological methods identified two dominant provenances: Triassic clastic rocks and Volgian suprasubduction volcanic rocks. The Middle Volgian–Early Berriasian age of the Imlekin Formation is specified. The geodynamic model proposed explains the change of the sources and direction of the sediment transport in the Volgian.