тектонічна будова

Relationship of the spatial distribution of seismicity with the tectonic structure of the Transcarpathian depression

In the paper discusses the features of long-term seismicity (1961-2010) the territory of Transcarpathian depression and separate seismoactive zones (A, B and C).  The relationship of these zones with the main tectonic elements of depression is set. It is proved that the boundary between zones A and B passes through Oash deep fault.

Deep structure of the north-western part of the Carpathian oil-and-gas bearing region based on integral interpretatiion of complex geologiocal and geophysical data

The report is devoted to an actual problem of studying the deep structure of the Carpathian region. Our research is based on creating a spatial integral seismic-gravity model. Gained results gave the opportunity to single out a number of lowered and raised blocks of the basement which correlate with the main tectonic units of the region and specify its geological structure. Further studying of the territory requires conduction of regional seismic investigation and its integral interpretation.