摘要
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。
Kalatongke Cu Ni deposit is of magmatic seperation type ore deposit occuring in orogenic belt far from craton.Based on systematic geological,geochemical and geophysical studies of the deposit is proposed the deep fault controling of basic rock—post emplacement magmatic sepesation and crystalization differentiation of magmatic ore—sussessive ejection model for the deposit.Geological,geochemical and geophysical marks which can be used as ore propecting guides are summed up and integrated information model for prospecting such ore deposits in Xinjiang is established.
出处
《地质找矿论丛》
CAS
CSCD
1998年第3期61-66,共6页
Contributions to Geology and Mineral Resources Research
