Abstract:Xiaoxinancha gold-copper deposit occurs in the contact between the Late Variscan diorite and Lower Palaeozoic Wudaoguo group The mineralizing types include gold bearing quartz-sulfide veins and concentrated veinlets The ore bodies are controlled by S-N-and NW-trending faults or fractures The deposit is magmatic hydrothermal origin
时俊峰. 小西南岔金铜矿床地质特征及成因机制[J]. 地质与资源, 1998, 7(4): 274-280.
Shi Junfeng. GEOLOGICAL CHARACTERISTICS AND MINEROGENEIC MECHANISM OF THE XIAOXINANCHA GOLD COPPER DEPOSIT. GEOLOGY AND RESOURCES, 1998, 7(4): 274-280.