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四川攀西(攀枝花-西昌)地区出露攀枝花、红格和白马三个赋含超大型钒钛磁铁矿床的镁铁-超镁铁质层状岩体。这些含矿岩体的独特之处在于:大量的块状和半块状矿石发育在岩体的偏下部位,不同比例的硅酸盐矿物(斜长石、辉石、橄榄石及磷灰石)和磁铁矿组成的韵律条带发育在偏上部位。这一韵律特征与南非布什维尔德
Sichuan Panxi (Panzhihua - Xichang) area revealed the mafic-ultramafic layered rock mass containing three super-large vanadium-titanium magnetite deposits in Panzhihua, Hongge and Baima. These ore-bearing rock masses are unique in that a large number of massive and semi-massive ores develop in the lower part of the rock mass. Different proportions of silicate minerals (plagioclase, pyroxene, olivine and apatite ) And the magnetite composed of prosodic bands developed in the upper position. This rhythm is characteristic of bushveld in south africa