Tourmaline populations studied from the Campanian–Maastrichtian part of the Ropianka (Upper Cretaceous-Paleocene) and Menilite (Oligocene) formations of the Polish Carpathians, represent a mixture of first-cycle and polycyclic grains. The tourmalines
view moreTo the east of the WaksmundPonice Dislocation Zone, the Beloveža Fm, as well as the part of the Ropianka Fm are tectonically reduced.
view moreDownload scientific diagram | Planktonic foraminiferids from the Gaj section. 1, 7 – Heterohelix striata (Ehrenberg), sample Gaj 5. 2 – Pseudotextularia elegans (Rzehak), sample Gaj 5. 3—6 ...
view moreLate Maastrichtian foraminiferids and diatoms from the Polish Carpathians (Ropianka Formation, Skole Nappe): a case study from the Chmielnik-Grabowka composite section. Acta Geologica Polonica,
view moreAbundant and taxonomically diverse foraminiferal assemblages of agglutinated, benthonic and occasional planktonic forms indicate a Middle Paleocene age for the upper part of the Ropianka Fm.
view moreZircon, tourmaline, rutile, garnet, staurolite and kyanite belong to the main constituents in both formations. Apatite is common in the Ropianka Fm., while the Menilite Fm. almost lacks this mineral. Furthermore, individual hornblende grains were found in the Ropianka Fm., while andalusite is present only in the Menilite Fm.
view moreApatite is common in the Ropianka Fm., while the Menilite Fm. almost lacks this mineral. Furthermore, individual hornblende grains were found in the Ropianka Fm., while andalusite is present only ...
view more17th Czech-Slovak-Polish Palaeontological Conference October 20–21, 2016, Kraków, Poland
view moreZircon, tourmaline, rutile, garnet, staurolite and kyanite belong to the main constituents in both formations. Apatite is common in the Ropianka Fm., while the Menilite Fm. almost lacks this mineral. Furthermore, individual hornblende grains were found in the Ropianka Fm., while andalusite is present only in the Menilite Fm.
view moreDownload scientific diagram | Species occurrence in the studied samples. For biozones see Fig. 5. from publication: Latest Maastrichtian foraminiferal assemblages from the Husów region (Skole ...
view moreAbundant and taxonomically diverse foraminiferal assemblages of agglutinated, benthonic and occasional planktonic forms indicate a Middle Paleocene age for the upper part of the Ropianka Fm.
view moreDownload scientific diagram | Sec tion of the Siedliska Mem ber at Siedliska with lo ca tion of the sam ple ana lysed Grain size: cl-clay, s-silt, vf-very fine sand, f-fine sand, m-medium sand, c ...
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