Геологічна природа Передкарпатського регіонального мінімуму сили тяжіння

Abstract

The has been considered he structure of the Precarpathian regional minimum of gravity pull and its connection with the Precarpathian depression. As to the regional minimum there has been defined the separate links that differ in their structure - Starosambirska, Boryslav-Peregynska, Peregyn-Kosmatska and Vorokhta-Grynjavska. Yt has been defined that the regional minimum was created as a result of the Earth's crust depression caused by the folding processes and accumulation of sedimentations folded in the area of hard stop of the Precarpathian fracture.

The couclusion has been made as to the further prospects of oil bearing capacity of the Precarpathians that can be related to the Starosambirska and Vorokhta-Grynjavska links of the regional minimum of gravity pull.