LITHOLOGIC-STRUCTURAL FEATURES OF THE SECTION OF UPPER CRETACEOUS–PALEOGENE BOUNDARY IN THE PARASKA THRUST SHEET REAR PART (KOROSTIV-VILLAGE AREA)

Authors

  • Milena Bohdanova
  • Oleksandr Kostiuk

Keywords:

Paraska thrust sheet, strike-slip fault, structure of imbrication, flysch deposits, Ukrainian Carpathians.

Abstract

The new data on the lithological composition of layers from the Upper Cretaceous– Paleogene сontact zone in the flysch strata, which is exposed in the rear part of the Paraska thrust sheet (left side of the Oriava-river, north-eastern outskirts of the Korostivvillage, Skole district, Lviv region), are given. Because of large-scale mapping, the ratio of individual layers of the section was analyzed and the structural features of this contact zone were determined. In general, the section reflects the structure of imbrication caused by lit-par-lit sliding of the layers. The section is complicated by a low-amplitude steepinclined left-sided strike-slip fault. We associate the lithological composition and the facial variability of deposits with the conditions of sedimentation, as well as the longitudinal and transverse tectonic zoning of the trough basin.

References

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Published

2018-12-27