沿云南哀牢山西侧九甲—安定大断裂带分布着若干超基性岩群,这些岩体常发育风化壳型镍、钴矿。由于超基性岩体中Co、Ni含量远高于其它地质体,因此分别以90×10-6、600×10-6圈定的Co、Ni异常既可以准确圈定超基性岩体边界,又可以明显地反映出风化壳型镍、钴矿信息。经资源潜力评价,哀牢山西侧寻找风化壳型镍、钴矿前景巨大。 A number of ultrabasic rock masses are distributed along the Jiutake-Andingtao fault zone on the west side of Ailao Mountain, Yunnan. These rock masses often develop weathered crust nickel and cobalt ore. Because the contents of Co and Ni in ultramafic rocks are much higher than other geological bodies, the abnormalities of Co and Ni delineated by 90 × 10-6,600 × 10-6 respectively can accurately delineate the boundaries of ultramafic rocks. Can clearly reflect the weathered shell nickel, cobalt ore information. The resource potential of the assessment, Ailao Mountain looking for weathering crust nickel, cobalt prospect great.