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前言太平山铁矿位于新余铁矿田东段,东邻良山铁矿,西与下坊铁矿寨口矿段毗连.矿层赋存于震旦系上部松山群杨家桥组下段.按正常层序,矿层上部为绿泥磁铁石英岩,下部为镜铁磁铁石英岩,直接顶板为绿泥千枚岩,直接底板为含磁铁绿泥绢云千枚岩.太平山铁矿现在的地层层序为倒转层序.1958年以来,对新余矿田各矿区矿体形态的认识,一直存在着“多层矿”与“单层矿”(即“红绸舞”)两种观点.在太平山铁矿勘探过程中,我们认识到,矿体的形态不过是地质构造作用形成的一种表象,而构造作用本身则是产
The Taipingshan Iron Mine is located in the eastern section of the Xinyu iron ore field, adjoining the Liangshan Iron Mine to the east and Xiazai Iron Mine in the west to the ore section of the Xiakou Iron Mine.The ore strata occur in the lower part of the Yangjiaqiao Formation of the Songshan Group in the upper part of the Sinian.According to the normal sequence , The upper part of the mine is green quartzite quartzite, the lower part is mirror iron magnet quartzite, the direct roof is chlorite phyllite, the direct bottom plate is magnesite green mud sericite phyllite, and the stratigraphic sequence of the Taipingshan iron mine is Inverted sequence. Since 1958, there have been two kinds of “multi-layer ore” and “single-layer ore” (ie, “red silk dance” In the exploration of the Taipingshan Iron Mine, we recognize that the shape of the ore body is only an appearance of the geological tectonics that is itself