ALEX STREKEISENSilicatemarble
The highestgrade assemblage in calcsilicate marbles is Cal + Qtz + Di. In contrast to dolomiterich rocks, there is very little overlap between the tremolite and the diopside field in calcite marbles. Wollastonite: wollastonite does not form in regional metamorphic rocks under closed system conditions. Even under granulite facies