The Kalatongke magmatic Cu-Ni deposit is situated in the northern Junggar orogenic belt.
喀拉通克岩浆型硫化铜镍矿床产于新疆北准噶尔褶皱带。
The new research methodology for delineating anomalies of concealed copper-nickel deposits combines the grey system theory with methods in terms of geology, geophysical exploration, and geochemical exploration.
该方法在新疆哈密研究区作了隐伏铜镍矿床预测试验,在找矿信息的采集中,选取了地质、物探、化探标志13个。