Zobrazeno 1 - 8
of 8
pro vyhledávání: '"Marcela Stárková"'
Autor:
Marcela Stárková, Vladislav Rapprich
Publikováno v:
Geoscience Research Reports. :97-102
Autor:
Renata Kadlecová, Jan Vít, Zuzana Skácelová, Marcela Stárková, Otmar Petyniak, Roland Nádaskay
Publikováno v:
Geoscience Research Reports. :103-117
Autor:
Marcela Stárková, Michal Hartman
Publikováno v:
Geoscience Research Reports. :159-164
Publikováno v:
Geoconservation Research, Vol 6, Iss 1, Pp 98-113 (2023)
Central Europe and the area of the UNESCO Global Geopark Bohemian Paradise have been affected by global tectonic events, especially during the last 500 million years. Volcanic phenomena are the most striking traces today of such past tectonic events.
Externí odkaz:
https://doaj.org/article/9380c81e7603439bad811dd32553a61a
Publikováno v:
International Journal of Earth Sciences. 104:1277-1298
The succession of Stephanian C lacustrine and fluvial facies of the Ploužnice member (Semily Formation) paleolake in the Krkonose Piedmont Basin (northern Czech Republic) preserved in borehole Sm-1 shows five types of soft-sediment deformation struc
Autor:
Vladislav Rapprich, Jan Balek, Marcela Stárková, Jan Valenta, Zuzana Skácelová, Lucia Fojtíková, Frantisek Stanek
Publikováno v:
Journal of GEOsciences. :169-181
The Permian pyroclastic deposits on the Principalek Hill SW of Vrchlabi (Czech Republic) were investigated by means of geological mapping and geophysics. The pyroclastic rocks are exposed in several small coherent outcrops, yet many interpretations a
Publikováno v:
Journal of GEOsciences. :163-180
*Corresponding author The Permian pyroclastic deposits of the Levin Volcanic Field within the Krkonose Piedmont Basin were studied in terms of volcanology. Pyroclastic rocks are exposed in two quarries and the study was supported with a 30 m deep bor
Publikováno v:
Geological Quarterly. 58
Mafic, monogenetic volcanism is increasingly recognized as a common manifestation of post-collisional volcanism in late Variscan, Permo-Carboniferous intramontane basins of Central Europe. Although identification of individual eruptive centres is not