Principles of large–scale prognosis for rare-metal mineralization in volcano-plutonic formations (with the aid of electronic computers)

1973 ◽  
Vol 15 (1) ◽  
pp. 80-88
Author(s):  
A.N. Yeremeyev ◽  
I.S. Modnikov ◽  
V.M. Pisarevskiy ◽  
L.V. Chesnokov
Keyword(s):  
Large Scale ◽  
Rare Metal ◽  
Rare Metal Mineralization ◽  
Electronic Computers

The Geological Characteristics and Potential Evaluation of Yunnan Zhenkang Luziyuan Mining Area

2014 ◽  
Vol 522-524 ◽  
pp. 1299-1302 ◽  
Author(s):  
Bin Xiao ◽  
Jun Li ◽  
Yu Hua Fan
Keyword(s):  
Large Scale ◽  
Mining Area ◽  
Wall Rock ◽  
Rare Metal ◽  
Metal Mining ◽  
Ore Bodies ◽  
Gravity Measurements ◽  
Rare Metal Mineralization ◽  
Lead Zinc ◽  
Resource Replacement

Luziyuan lead zinc iron metal mining area is located in the south of Baoshan-Zhenkang lead, zinc, mercury, rare metal mineralization belt of the southwest Sanjiang metallogenic belt.According to the mine tunnel drilling and logging data, that the ore bodies are controlled by strata and faults, symbiosis and Dali rock, limestone, near ore wall rock skarnization strongly, the research shows that the deposit belongs to sedimentary transformation - skarn Pb Zn Fe polymetallic deposit. [ Mining area within the range of 1:50000, 1:50000 gravity measurements of soil geochemical survey, combined with the large scale mapping of data discovery lead zinc iron copper resources are expected to find in the eastern Luziyuan area Mangxi - Head Mountain Luojiazhai resource replacement area.

scholarly journals Золотая минерализация штокового рудного поля (Магаданская область)

2021 ◽  
pp. 13-29
Author(s):  
A. N. Glukhov ◽  
◽  
M. I. Fomina ◽  
E. E. Kolova ◽  
◽  
...  
Keyword(s):  
Volcanic Belt ◽  
Rare Metal ◽  
Geological Structure ◽  
Physicochemical Conditions ◽  
Epithermal Mineralization ◽  
Ore Bodies ◽  
Mineral Associations ◽  
Rare Metal Mineralization ◽  
Chukotka Volcanic Belt ◽  
Formation Conditions

The authors briefly characterize the geology and structure of the Shtokovoye ore field attached to the area where the Khurchan-Orotukan zone of tectonic-magmatic activation overlays the structures of the Yana-Kolyma ore-bearing belt. Studied are mineral associations and physicochemical conditions of gold ore bodies, located both in granites and in hornfelsed sedimentary masses. By the main features of its geological structure, ore composition, and physicochemical formation conditions, the Shtokovoye ore field mineralization corresponds to the "depth" group of the gold-rare-metal formation, analogous to the Butarnoye, Basugunyinskiye, Dubach, and Nadezhda occurrences. Its ores are peculiar in the late epithermal mineralization, which is associated with the Okhotsk-Chukotka volcanic belt and overlays the sinaccretional gold-rare-metal mineralization.

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