FEATURES OF THE HYDROCARBON TRAPS' CONSTRUCTION, CONFINED TO THE ANTICLINE INVERSION STRUCTURES OF THE KARAKUL`S ROLLER
The seismic investigations proved the existence of the zone of the mezo-cainozoic sediment discontinuity within the northern circumference of the Karakul`s roller. The conditions of the formation of these zones are justified with the post-rift processes and energization of the intraplate tension during the Alpine epoch of folding. Tectonic movements within the faulted zones can serve as a formation cap for the inversion structures, found within Karakul's roller. The subsequent investigations of the Karakul`s roller territory by the high-resoluted seismic exploration can be useful for the discovery of the new oil and gas fields.