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喀拉通克铜镍矿床为产出于造山带且远离克拉通的岩浆熔离型铜镍矿。通过系统研究矿床的地质、地球物理及地球化学特征，提出深大断裂控制基性岩产出，含矿基性岩浆侵位后熔离—结晶分异和矿浆依次贯入的成矿模式，总结出找矿的地质、地球物理及地球化学标志，最后给出了综合信息找矿模型。
The Kalatongk copper-nickel deposit is a magmatic eruptive type Cu-Ni deposit that is either derived from orogenic belt and away from craton. Through systematically studying the geologic, geophysical and geochemical characteristics of the ore deposit, the authors put forward the metallogenic model that controlled the production of basic rocks by deep faults and separated the melt-crystallize differentiation and the ore-pulp in turn after emplacement of the ore-bearing basic magma, and concluded Geological, geophysical and geochemical signs of prospecting are given, and finally a comprehensive information prospecting model is given.