The hongqiling cu - ni ore deposit is located to the northern flank of a contacting zone ( the huifahe fault systems ) between the north china platform and the jilin - heilongjiang syncline system 摘要红旗岭铜镍矿床地处华北地台与吉黑地槽系接触带辉发河断裂北侧。
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The level of contaminants was increase in order of jinchuan ( hongqiling ) < jianchaling < east huangshan ( kalatongke ) . proterozoic is important evolution period in forming of nickel - copper deposits . 4 中国含铜镍硫化物矿床按受混染程度由弱到强排列为金川(红旗岭)煎茶岭黄山东(喀拉通克) 。