Quantitative calculation of trace element content for the residue after partial melting suggests that intermediate-mafic granulites outcropped in the Dabie orogen are not the residue of partial melting.
Quantitative calculation of trace element content for the residue after partial melting suggests that intermediate-mafic granulites outcropped in the Dabie orogen are not the residue of partial melting.
残留相微量元素定量计算结果表明，大别山现今出露的中基性麻粒岩不是部分熔融后形成的残留体。