Using the tracer ability of petro-geochemistry,the paper discusses on source characteristics and magma evolution of the high-Mg volcanic rocks.
利用岩石地球化学的可示踪性，研究了高镁火山岩浆的源区特征、岩浆演化。
参考来源 - 宾川—程海二叠纪高镁火山岩的岩石地球化学及含矿性·2,447,543篇论文数据，部分数据来源于NoteExpress
The idea that quartz vein is the last product of magma evolution has been widely accepted for a long time.
关于地壳中广泛分布的石英脉体的成因，传统的岩浆演化最终产物的观点，长期以来被广泛接受。
They can be used to track the mantle structure, degassing history, inhomogeneity, magma evolution and the genesis of natural CO2.
它们可对地幔结构、地幔脱气历史、大陆地幔不均一性、幔源岩浆演化和CO2天然气成因等研究提供独特的示踪作用。
Using the tracer ability of petrogeochemistry, the paper discusses on source characteristics and magma evolution of the high-Mg volcanic rocks.
利用岩石地球化学的可示踪性，研究了高镁火山岩浆的源区特征、岩浆演化。
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