The emplacement and evolution of magma are not only a trend of material evolution but also a process of energy release and transfer.
岩浆的侵位和演化过程不仅仅表现为物质上的演化趋势，而且也是能量的释放和转移过程。
The mechanism of this anti-order magmatic evolution is mainly caused by the separate crystallization of plagioclase in a high-level magma chamber.
这种反序岩浆演化的机制主要是由于斜长石在高位岩浆房中的分离结晶所致。
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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