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红土型金矿不一定规模大、品位低、粒度细; 而更多的是中、小型规模, 品位可高可低, 粒度可粗可细; 矿床分布不局限在现代的低纬度地区, 而应具体分析古地理和古气候; 大地构造环境不强调稳定区和准平原化, 活动带中一些相对稳定的地区也能成矿; 红土化发育程度不要求很高, 只要达到次强度、甚至中度富铝化即可。正确认识这些基本地质特征和成矿条件,对研究红土型金矿的成矿理论和找矿实践、甚至对选冶方法和流程, 均具有重要的指导意义。
Lateritic gold is not necessarily large in scale, low in grade and fine in grain size; more is in medium and small scale, with high and low grade, coarse and fine grain size; deposit distribution is not confined to the modern low latitudes, but should Paleogeography and palaeoclimate are analyzed in detail; the stable environment and quasi-plains are not emphasized in the tectonic setting of the tectonism, and some relatively stable areas in the active zone are also mineralized. The degree of development of the laterite is not very high, so long as the secondary intensity is reached, or even moderately rich Aluminum can be. Correct understanding of these basic geological features and metallogenic conditions has important guiding significance for studying the metallogenic theory and prospecting practice of lateritic gold mines, and even for the methods and processes of metallurgy and metallurgy.