Shi Junfeng. GEOLOGICAL CHARACTERISTICS AND MINEROGENEIC MECHANISM OF THE XIAOXINANCHA GOLD COPPER DEPOSIT[J]. Geology and Resources, 1998, 7(4): 274-280. DOI: 10.13686/j.cnki.dzyzy.1998.04.005
Citation:
Shi Junfeng. GEOLOGICAL CHARACTERISTICS AND MINEROGENEIC MECHANISM OF THE XIAOXINANCHA GOLD COPPER DEPOSIT[J]. Geology and Resources, 1998, 7(4): 274-280. DOI: 10.13686/j.cnki.dzyzy.1998.04.005
Shi Junfeng. GEOLOGICAL CHARACTERISTICS AND MINEROGENEIC MECHANISM OF THE XIAOXINANCHA GOLD COPPER DEPOSIT[J]. Geology and Resources, 1998, 7(4): 274-280. DOI: 10.13686/j.cnki.dzyzy.1998.04.005
Citation:
Shi Junfeng. GEOLOGICAL CHARACTERISTICS AND MINEROGENEIC MECHANISM OF THE XIAOXINANCHA GOLD COPPER DEPOSIT[J]. Geology and Resources, 1998, 7(4): 274-280. DOI: 10.13686/j.cnki.dzyzy.1998.04.005
GEOLOGICAL CHARACTERISTICS AND MINEROGENEIC MECHANISM OF THE XIAOXINANCHA GOLD COPPER DEPOSIT
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
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