Zincoberaunite is an iron and zinc phosphate mineral, the Zn analogue of beraunite.
It was first described by Chukanov et al. for an occurrence in Hagendorf Sud pegmatite in Germany.
It appears in two paragenesis, as an alteration of other phosphates in pegmatites: in one with jungle, phosphophyllite and mitridatite and in another with flurlite, plimerite, beraunite rich in zinc, schoonerite, parascholzite, robertsite and altered phosphophyllite.
However, it is likely that a detailed study of the zinc-rich beraunite specimens will allow locating other localities for the zincoberaunite.
In the type locality it appears as pale gray capillary microcrystals forming silky-looking aggregates.