Figure 8
From: Carbonation and serpentinization of diopsidite in the Altun Mountains, NW China
Mineral compositions of the pyroxenes in the Yushishan diopsidites. The CaSiO3(Wo)–MgSiO3(En)–FeSiO3(Fs) diagram (modified from Morimoto et al.48) shows that all pyroxenes are diopsides.
