岩浆源区再循环玄武质洋壳的存在可能是该区超大型钒钛磁铁矿床形成的根本原因。
The existence of recycled basaltic oceanic crust in the axial zone of mantle plume may be the key of the formation of giant V-Ti-magnetite deposits.
运用近年来国内外广泛采用的特征矿物物源示踪法来研究长江三峡的贯通，并选择攀枝花钒钛磁铁矿床中的钛磁铁矿作为示踪矿物进行了探讨。
This paper presents a research for the origin of Three Gorges by using the approach of diagnostic minerals tracing which has been well developed globally in recent several years.
可把此矿床定名为次火山水热石榴子石-透辉石-磁铁矿矿床。
The ore deposit can be named as subvolcanic hydrothermal garnet-diopside-magnetite deposit.
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