@ARTICLE{Panek_Emil_Mineralogical_2001, author={Panek, Emil and Pawlikowski, Marek}, number={No 3}, journal={Gospodarka Surowcami Mineralnymi - Mineral Resources Management}, pages={53-71}, howpublished={online}, year={2001}, publisher={Komitet Zrównoważonej Gospodarki Surowcami Mineralnymi PAN}, publisher={Instytut Gospodarki Surowcami Mineralnymi i Energią PAN}, abstract={The aim of the study was to determine mineralogical composition of carpathian sandstones in order to define petrographic composition of the source material areas. The mineralogical composition of the carpathian flysh sandstones collected in six sampling sites was established. The samples collected in the profiles no I and II in Beskid Śląski represent istebnaiańskie sandstones. The other four sampling sites were located in Beskid Żywiecki, Gorce and Beskid Śądecki and represent magurskie sandstones. Tree samples of rock material were collected in reach sampling profile from the BC horizon. The sandstones contain various amounts of quartz, potassium feldsaprs, plagioclase, fragments of sedimentary, magmatic and metamorphic rocks, muscovite, biotite, carbonates, glauconite, heavy minerals, organic matter and binder. There are considerable differences in mineral composition of the sandstone samples taken from six profiles as well as from the same profile. The istebniańskie sandstones contain average higher amounts of metamorphic and sedimentary rocks than the magurskie sandstones. On the contrary, the magurskie sandstones contain higher amounts of quartz.}, type={Artykuł}, title={Mineralogical and petrographic variability of sandstones from Westem Beskidy Mts. between Stożek and Czantoria mountain range in Silesian Beskid and Jaworzyna Krynicka in Sądecki Beskid}, URL={http://journals.pan.pl/Content/132751/PDF/6_GSM_17_3_2001_Panek_Zmiennosc.pdf}, keywords={Carpathian flysh, Magura and Istebna sandstones, mineralogical composition, quartz, sedimentary environment, metamorphicand magmatic rocks, binders, spatial variability, Westem Beskidy Mts}, }