Different Origins of the Fractionation of Platinum-Group Elements in Raobazhai and Bixiling Mafic-Ultramafic Rocks from the Dabie Orogen, Central China
Figure 2
Chondrite-normalized REE patterns (a) and spider patterns (b) of Raobazhai mafic-ultramafic rocks (chondrite and primitive mantle values are from [9]).
