矿物学及地球化学结果表明大东山是一个高分异的I 型花岗岩岩体。
Mineralogical and geochemical features suggest that the Dadongshan granites are highly fractionated I-type granites.
组成玲珑花岗岩基的各个岩体具有不同的磁化率各向异性度。
Deferent plutons composing Linglong composite granitoid batholith have deferent degrees of anisotropy of magnetic susceptibility.
花岗岩形成巨大的岩体。
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