Abstract：The south margin faulted zone of Altun Mountain in Xinjiang is a regional upper mantle deep structure,along which numerous basic-ultrabasic complex bodies are distributed.The elements of Cu,Au,Pt and Pd are concentrated in the late stage of magmatic crystallization and differentiation.With later tectonic hydrothermal process,commercial copper-gold-platinum-palladium deposits are formed in Qingshuiquan and other places.There is a great potential for the exploration in Altun area.
刘国范, 朱广彬, 陈金铎, 杨振军, 秦爽. 新疆阿尔金南缘断裂带铜金铂钯贵金属矿床特征及成因[J]. 地质与资源, 2005, 14(1): 28-32.
LIU Guo-fan, ZHU Guang-bin, CHEN Jin-duo, YANG Zhen-jun, QIN Shuang. GEOLOGY AND METALLOGENESIS OF THE PRECIOUS METAL DEPOSITS IN THE SOUTH MARGIN FAULT ZONE OF ALTUN MOUNTAIN, XINJIANG. GEOLOGY AND RESOURCES, 2005, 14(1): 28-32.
2005, Vol. 14 
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