The systematic changes of the igneous rock series and the genesis types have reflected polycyclic transference features of the crust and mantle materials.
火山岩系列和成因类型的系统变化，反映了多旋回壳幔物质迁移特证。
The systematic changes of the igneous rock series and the genesis types have reflected polycyclic transference features of the crust and mantle materials.
火山岩系列和成因类型的系统变化，反映了多旋回壳幔物质迁移特证。
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