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诺里尔斯克和北方河流地区早在1932年便被划为铜-镍和铁矿矿化作用地段。后来的工作确定,局部具工业价值的含矿分异侵入体不仅沿通古斯地向斜西缘叶尼塞河右岸发育,而且也沿该地向斜的北缘和东缘发育,这两个边缘近年来也发现了一系列受深断裂带控制的局部含工业铜-镍矿的分异侵入体。这个从西、北、东三面环绕着通古斯地向斜的宽广的地带,现在有充分的根据能划为具有独特的金属矿化、强烈的地质构造变动和基性与超基性岩浆作用的一个新的巨大的叶尼塞-哈坦加镍矿省。
Norilsk and the Northern Rivers were delineated as copper-nickel and iron mineralization back in 1932. Subsequent work identified that the locally industrialized ore-bearing divergent intrusions developed not only along the right bank of the Yenisei River in the syncocentially western side of the Tunguska but also along the syncline north and east margins of the two margins In recent years, a series of differentiated intrusions containing local industrial copper-nickel ore under the control of deep fault zones have also been discovered. This extensive zone of synclines that surround the Tunguska from the west, north and east is now well-founded for its unique metallogenetic, intense geological tectonics and basic and ultrabasic magmatisms The new huge Yenisei-Hatanga nickel mine province.