The Polish Outer Carpathians (POC) form part of the arcuate Carpathian mountain system,
that extends over more than 1300 km from the Danube valley in Austria to the Danube valley …

The principal source rocks in the Outer Carpathians are organic‐rich shales in the
Oligocene to Lower Miocene Menilite Formation. The average total organic carbon (TOC) …

The purpose of this chapter is to provide the general overview of the stratigraphy and
tectonics of the Polish, Ukrainian, and adjacent parts of the Slovakian Outer Carpathians …

The sedimentary basins of the Outer Carpathians are regarded as the remnant oceanic
basins that were transformed into the foreland basin. These basins developed between the …

Multiple petroleum systems occurring in different tectonic elements of the Polish and
Ukrainian parts of the Flysch Carpathians, their foredeep, and the Paleozoic–Mesozoic …

Mineral liberation analysis (MLA) is a computer-automated technique used to identify and
quantify minerals with scanning electron microscopy (SEM) based on backscattered electron …

Over the last 65 Ma, our world assumed its modern shape. This timespan is divided into the
Palaeogene Period, lasting from 65 to 23 Ma and the Neogene, which extends up to the …

This paper presents an insight into the geology of the area surrounding the ODDP proposed
drilling site, and the structural development of the Carpathians in post-Palaeogene times …

The Silesian Series deposited in the proto-Silesian and Silesian basins and preserved
within the Silesian Nappe, represents most complete continuous basinal sedimentary …

Textural and structural features of submarine mass density flow sediments are a record of
depositional flow evolution and hydrodynamics. Record of changes in such flow movement …