There is, for me, a more significant problem with the spherical crystals in a granulite facies rock (prismatine rock from Waldheim). Spherical crystals in larger spherical crystals and bulk rock are not rare – I think they are very characteristic features of this unusual rock. According to geologists, this rock is usually formed by exhumation and involving melting due to decompression. And that is the problem! The formation of spherical crystals in a static state is nearly impossible. Necessary is a separation of the equilibrium melt from the corroded spherical crystals. If not such separation happens, the spherical crystals will obtain her equilibrium habitus. I assume at least a two-stage evolution. Crystallization of the bulk rock, maybe from the decompression melt and input of a fast-rising very low viscous melt from a greater deep carrying the spherical crystals (high quartz with zircon, zircon, garnets, feldspars, corundum, and many others) and more exotic phases like coesite and stishovite. The two-stage evolution is characterized by a normal metamorphic crystallization and an input of a more pegmatite-forming melt from great deep, like the Starkoč abyssal pegmatite in the Gföhl unit (characterized by HT/HP rocks) in the Bohemian Massif (Jan Cempirek and Milan Novák, 2010). In this pegmatite, I have also found a large number of spherical crystals. Is there any other explanation? Karl Hermann Scheumann: Das Kornerupingestein von Waldheim in seinem genetischen Zusammenhang (1960) discussed already the meaning of a pegmatitic phase for the formation of the prismatine rock (however, in a bit of old-fashioned manner).

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