地質(zhì)勘查和礦床研究結(jié)果表明,我國(guó)鐵礦床類型齊全,世界上已發(fā)現(xiàn)的鐵礦成因類型在我國(guó)均有發(fā)現(xiàn),除前寒武紀(jì)硅鐵建造風(fēng)化殼型鐵礦外,均探明了一定的儲(chǔ)量,其中以沉積變質(zhì)型為主,儲(chǔ)量占57.8%,居各類型鐵礦床之首,其次是接觸交代-熱液型(占12.7%)、巖漿晚期型(占11.6%)、沉積型(8.7%)、與火山-侵入活動(dòng)有關(guān)型(占4.7%)、風(fēng)化淋濾型(占1.1%),其他類型占3.4%。與世界不同之處在于我國(guó)接觸交代-熱液型和巖漿型儲(chǔ)量占的比例較高.
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