这些表明不同稀土特征的萤石来自相同的源区，稀土成矿流体与碳酸岩和正长岩岩浆存在密切联系。
This suggests that the different REE fluorites were products of the same source, and REE ore-forming fluids were related to carbonatite and syenite magmas.
相对于碱性橄榄玄武岩，白榴石碱玄岩来自于更加富集的地幔源区，其地幔的部分熔融程度相对较低。
Leucite tephrite was derived from the more enriched mantle source with lower degree of partial melting of mantle source than alkaline olivine basalt.
该矿床的成矿物质具深源性，主要来自上地幔或下部地壳，是一种火山岩区剪切带蚀变岩型金矿床。
The deposit is a shear belt-hosted altered rock-type gold deposit in the volcanic rock area.
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