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比较纯的透辉石出现于某些热变质的硅质白云岩和矽卡岩中,产于各种各样的岩浆岩中,广泛分布于基性和超基性岩中,是一种常见的矿物。透辉石的分了式:CaMg(Si_2O_6),理论
More pure diopside occurs in some thermally altered siliceous dolomites and skarns, is produced in a variety of magmatic rocks and is widely distributed in both mafic and ultrabasic rocks and is a common Minerals. Diopside sub-type: CaMg (Si_2O_6), theory