22008 - Top Rare Selenopeltis aff. gallica Lower Ordovician Trilobite Fezouata Fm Teeth Troilite not surrounded by schreibersite

Troilite not surrounded by schreibersite

The different Geological Formations that make up the orography of the Cretaceous in the South East of Morocco have been mostly treated in an undifferentiated and not too accurate way by collectors

all per mil)

Full reference: A

22008 - Top Rare Selenopeltis aff. gallica Lower Ordovician Trilobite Fezouata Fm Teeth Troilite not surrounded by schreibersiteImpressive specimen of the genus Selenopeltis, It comes from the Lower Ordovician of the Famous Fezouata Formation. Finest Grade. The Fezouata Formation occurs in the lower part of the Lower to lower Middle Ordovician Outer Feijas Group, in the western, central and eastern Anti Atlas Mountains, southern Morocco (Destombes et al. 1985; Gutierrez Marco & Martin 2016). It comes from The Konservat Lagersttten of Lower Fezouata Fm that spans the entire