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该矿床位于康滇地轴中段菜子园东西向断裂带南侧。矿床的主要有益元素镍呈类质同象代换磁铁矿中低价铁形成铁镍磁铁矿。铁镍磁铁矿在我国属首次发现。该矿呈星点状、网脉状等形态赋存于镁质超基性岩蚀变生成的蛇纹岩中。本文主要介绍该矿床的地质特征和富集规律。我们在工作中得到我队许多同志的热情帮助,并参阅了黄荣章、杨本锦等同志编写的有关的地质评价报告,苏世清同志帮助清绘插图,在此一并致谢。
The deposit is located on the south side of the east-west fault zone of CaiZi Yuan in the middle axis of Kangdi-Dianxi. The main beneficiary element of the deposit is similar in the same type of nickel instead of magnetite in the formation of low-cost iron-nickel magnetite. Iron-nickel magnetite is the first discovery in our country. The ore was a star-shaped, reticular and other forms occur in magmatic ultrabasic rock alteration generated serpentinite. This article mainly introduces the geological characteristics and enrichment law of this deposit. We have been warmly assisted by many comrades in our team during our work. We have also read the relevant geological evaluation reports prepared by Huang Rongzhang, Yang Benjin and other comrades. Comrade Su Shih-ching helped clear the illustrations and thank you for this.