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以青海肯德可克、新疆梧桐沟-尖山、陕西大西沟和海南石碌四个铁矿床为例,讨论了层控铁矿的动力成矿作用。原始沉积岩石或矿石所含各种组分,在动力作用下发生分异、重新组合,或在动力的压泌作用下使某些活动组分离去,从而导致原有铁质在有利的构造部位(通常是受力较强的部位)相对聚集而成矿,或使贫矿石变富。
Taking the four gold deposits of Kendakeg in Qinghai Province, Wutonggou - Jianshan in Xinjiang Province, Daxigou in Shaanxi Province and Shilu in Hainan Province as examples, the dynamic mineralization of strata - controlled iron ore is discussed. The original sedimentary rock or ore containing various components, under the action of the power of differentiation, re-combination, or under the action of the dynamic pressure of certain activities leaving the composition, resulting in the original iron in the favorable structural parts (Usually a strong part of the site) relative to the accumulation of mineralization, or enrich the poor ore.