Liu Bin, Yu Changtao. THE METALLOGENIC MODEL FOR MAOLINGVEINLET-DISSEMINATED GOLD DEPOSITIN THE SOUTH LIAONING[J]. Geology and Resources, 1994, 3(2): 103-106. DOI: 10.13686/j.cnki.dzyzy.1994.02.004
Citation:
Liu Bin, Yu Changtao. THE METALLOGENIC MODEL FOR MAOLINGVEINLET-DISSEMINATED GOLD DEPOSITIN THE SOUTH LIAONING[J]. Geology and Resources, 1994, 3(2): 103-106. DOI: 10.13686/j.cnki.dzyzy.1994.02.004
Liu Bin, Yu Changtao. THE METALLOGENIC MODEL FOR MAOLINGVEINLET-DISSEMINATED GOLD DEPOSITIN THE SOUTH LIAONING[J]. Geology and Resources, 1994, 3(2): 103-106. DOI: 10.13686/j.cnki.dzyzy.1994.02.004
Citation:
Liu Bin, Yu Changtao. THE METALLOGENIC MODEL FOR MAOLINGVEINLET-DISSEMINATED GOLD DEPOSITIN THE SOUTH LIAONING[J]. Geology and Resources, 1994, 3(2): 103-106. DOI: 10.13686/j.cnki.dzyzy.1994.02.004
THE METALLOGENIC MODEL FOR MAOLINGVEINLET-DISSEMINATED GOLD DEPOSITIN THE SOUTH LIAONING
Maoling gold deposit,located in the southwest of Liaodong Peninsula, discovered in 1985, is a giant veinlet-disseminated ore with low grade. The ore bodies are auriferous quartz veinlets and-arsenopyritized-pyritized sericite phyllite or schist. Au grade ranges from 3 to 5g/t. The country rock is the second member of Gaixian formation. Magmatic activities were common in the area.
DownLoad: