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Olistostrome horizons in the Oligocene deposits of the south-western part in the Bytlya-Svydovets subcover of the Krosno nappe or in so-called Pre-Duklya folds are described in a number of works. There is not enough information about olistostrome in the northern part of the Krosno nappe in its Turka subcover and in the outer part of the Duklya-Chornohora nappe (Stavniany subcover). In the mentioned tectonic units olistostrome is localized in the Lower Verkhovynian deposits of Oligocene above the marker bed of stripped limestones in the region of the Smozhe populated area of the Skole district of the Lviv Region, Torun and Lopushna of the Mizhgirria region of the Transcarpathian Region as well as near Lyuta Village of the same region. Matrix is mainly composed by the grey carbonate flysh of the Krosno lithotype. Olistostrome horizons are presented by strongly crumped chaotic non-sorted formations. In its composition also are present more ancient rocks than matrix, olistolites of the Upper Cretaceous-Lower Oligocene age as well as redeposited rocks formed as a result of washout of more ancient deposits. Some geologists consider, according, to M. G. Leonov hypothesis (1978), that olistolites came off the front part of the Duklya nappe during its overthrusting to the north-east. Materials collected during geological surveys and later observations deny such a mechanism. This is proved by the following: a) overthrust of the Duklya nappe couldn’t cause the formation of the Krosno olistostrome. Because olistostrome is also fixed in Oligocene of the Stavniany subcover of the given nappe of the Lyuta Village and the Mlaky ravine in the section of the Lyuta River. b) Olistostrome is traced at the strathigraphic level at a relatively narrow time interval. It means that sources of removal of olistolites were functioning not so long that contradicts the thesis on the permanent overthrusting movement. c) If olistostrome was caused by the given overthrust, so it would (and olistolites) be observed continuously, but not discretely. d) In sandstones of-the Lower Verkhovynian subsuite the presence of nummulites was fixed, and in argillites of Oligocene the microfauna of Cretaceous-Eocene age – this in the evidence of the washout event. e) Over olistostrome are developed normal bedded high sections of-the Lower Verkhovynian subsuite, thus the overthrusting of the scales in Oligocene was absent. f) In the composition of the Bytlya olistostrome are present rocks that are absent in the composition of Duklya-Chornohora nappe. In the light of data mentioned above, the alternative thesis about cordillera as a source of removal of olistolites is rather grounded and non-alternative. It is possible that as sources of removal was a number of islands that were uplifted higher that sea level at the beginning of the Upper Verkhovynian time. In places the tongues of olistostromes into the Turka sub cove olistolites in the Smozhe and Torun Village possibly due to the presence of long alluvial fans. It is probable that cordillera occurred at the boundary between the Krosno and Dusynian basins of sedimentation that differed by the conditions of sediment forming that was manifested by the presence of two lithotypes of Oligocene of Krosno and Dusynian.

The objective of this study is to analyze the influence of the Pokuttia deep fault on tectonics and the oiland gas-bearing structures in the southeastern part of the Ukrainian Carpathians. Methodology. It is presented in a detailed complex analysis of the geological-geophysical data in the given area. Results. The influence in the Pokuttia deep fault on the flysch structure has revealed itself in the Boryslav-Pokuttia nappe as a series of dislocations with a break of continuity at the northeastern orientation at the boundary between the Hutsulkyi and Boikivskyi segments with the structures horizontally displaced 10 km off and up to 1.5 km vertically-left-strike slip fault. In the Skyba nappe this is truncation of its front part of the Hutsulskyi segment. In the Dukla-Chornohora nappe and the Bitlya-Svydovets sub-nappe these are sigmoid curvature of their parts in the fault zone with amplitudes of horizontal displacements of up to 10 km. As a result, the Krasnoshora and Hoverla units are joined into a single sub-nappe, and the thrust-folds of the Bitlya-Svydovets sub-nappe to a considerable extent are overlapped by it and by the Skupiv subnappe. Owing to post-overthrusting vertical movements the Hutsulskyi segment was uplifted during Pliocene-Pleistocene. The rise of the area with the Duklya-Chornohora nappe was the most intensive. The structures of the Bitlya-Svydovets sub-nappe are fragmentally outcropped from under it. In the territory of Romania the nappes structurally correspond from the north-the thrust-sheet with olistostrome Slon in the Lower Verkhovyna deposits of Oligocene, and from the south-tectonic units Toroklezh and Makla. The Pokuttia fault displaces the Precarpathian regional minimum (amplitude of about 10 km), and the Uzhok deep fault with the signs of right-shift. There is a perceptible impact of the Pokuttia fault on the sub meridional Radekhiv-Viktoriv fault. Sites of intersections of the mentioned faults, so-called knots, if the traps are available, are known to be favourable zones for hydrocarbon accumulation on commercial scales. In the light of new data on the geological structure of the region, the perspective estimate is raised for the distinguished structures Vorohta-Yasynia (Lazeshchynska, Yasynska and Voronenkivska), as well as Semakivska and Hryniavska, where commercial influxes of hydrocarbons were obtained. This observation also concerns the structures of the basement of the Lopushna subzone of the outer zone of the Carpathean Foredeep under the overthrust of the Carpathians. Scientific novelty. For the first time, using new geological data it was possible to prove the influence of the Pokuttia fault in the zone of its action in a form of the left-strike-slip on the structures of the flysch cover. The structural parallelization of the Bitlya-Svydovets sub-nappe of the Krosno nappe of the Ukrainian Carpathians was carried out with the tectonic units of the Romanian Eastern Carpathians. Interaction of the given fault with the Precarpathian regional minimum and the Uzhok deep fault ha...