In Czech Republic, this form of zircon is a component of the U-Zr assemblage on the peneconcordant stratiform deposits in sandstones of northern Bohemia. Characteristic of this zircon is its metacolloidal to gel nature and other physical properties (low specific gravity, low aggregate hardness, and low refraction). It is so far known only from a few localities all over the world such as Wind River Formation in Wyoming. Does anyone know of a similar type of mineralization?