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红格镁铁-超镁铁层状侵入体位于峨眉山大火成岩省中部,赋存的超大型钒钛磁铁矿矿床是仅次于攀枝花矿床的我国第二大岩浆型钒钛磁铁矿矿床。该矿床主要的含矿层位为下部超镁铁岩带部分,与世界其他典型的含磁铁矿层状岩体如Skaergaard侵入体和Bushveld杂岩体存在明显的区别(磁铁
The red-grid mafic-ultramafic layered intrusions are located in the middle of the Emeishan large igneous province, and the super-large vanadium-titanium magnetite deposit is the second largest magmatic vanadium-titanium magnetite deposit in China only after the Panzhihua deposit. The main ore-bearing layer of the deposit is the lower part of the ultramafic belt, which is obviously different from other typical magnetite-bearing stratigraphic rocks such as the Skaergaard intrusion and the Bushveld complex (magnets