Browsing by Subject "Gogolin Formation"
Now showing 1 - 1 of 1
- Results Per Page
- Sort Options
Item type:Article, Access status: Open Access , Nowe jednostki litostratygraficzne w randze warstw w obrębie formacji gogolińskiej (trias środkowy) na Śląsku Opolskim(Wydawnictwa AGH, 2009) Kowal-Linka, MonikaThe Zakrzów Crinoidal Limestone Member is subdivided into the three subordinate units: the Krapkowice Pelitic Limestone Bed built of thin-bedded, wavy-bedded and crumpled marly pelitic limestones, the Dąbrówka Bioclastic Limestone Bed consisting of thick- to medium-bedded, cross-bedded bioclastic limestones (crinoidal), the Podbór Bioclastic Limestone Bed built of thin- to medium-bedded bioclastic limestones, pelitic limestones and intraformational conglomerates. The lower part of the Skała Marl Member consisting locally of the intraformational conglomerate with big intraclasts covered by the intraformational conglomerate with small intraclasts is designed as the Kocina Intraformational Conglomerate Bed. The Emilówka Cellular Limestone Member is subdivided into the two subordinate units: the Karłubiec Bioclastic Limestone Bed built of thin-to medium-bedded bioclastic and pelitic limestones and the Otmęt Marly Limestone Bed consisting of strongly porous, thin-bedded marly limestones (dedolomites).
