Naziv vsebine
Concretion with Chonetoid Brachiopod and Geochemical Halos
Site
Central Southern Karavanks.
Notes
Reddish specks in the concretion are interpreted as pyrite pseudomorphs formed under localized reducing conditions linked to organic decay, later oxidized to hematite and partially hydrated to limonite during burial diagenesis or weathering. C3 - P1.
