对我国矽卡岩铁矿找矿标志的几点认识

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矽卡岩铁矿床是内生金属矿床中的一个重要成因类型.这种类型矿床在我国分布广、盲矿多、品位富,并伴生有多种元素可综合利用,为重要的开采对象之一.在毛主席无产阶级革命路线指引下,建国以来,特别是无产阶级文化大革命以来,地质战线广大职工大力开展普查找矿工作,使矽卡岩型铁矿的老矿区规模不断扩大,新矿区不断发现.这种类型矿床在我国具有广阔的找矿前景.据不完全统计,我国矽卡岩铁矿约占全国铁矿总储量的14.3%(1970年资料),而 Skarn iron deposit is an important genetic type in endogenous metal deposits, which are widely distributed in our country, have many blind mines, are rich in grade, and are associated with a variety of elements that can be comprehensively utilized as important mining targets I. Under Chairman Mao’s proletarian revolutionary line and since the founding of the People’s Republic of China, especially since the Great Proletarian Cultural Revolution, the general staff on the geological front vigorously carried out surveys and prospecting work to keep the size of the old skarn iron ore mine expanding. The new mining area According to incomplete statistics, China’s skarn iron ore accounts for about 14.3% of the total reserves of iron ore in the country (data in 1970), and it has been found that this type of deposit has a vast prospecting prospect in our country
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