AbstractThe forming of each deposit has its objective and natural conditions. Different deposits have different types because their conditions and environments are different. This paper analyzed and discussed the cause of Shangping tungsten deposit. Firstly, it is the district background. Secondly, it is the geological characteristics and the age of the deposit. We think that the deposit is the zoning deposit of intermittently reverse precipitation from the pegmatite petrography to the hydrothermal solution stage gradually from the whole developing process. And this is a more complicated high temperature hydrothermal solution deposit of (FeMn) WO4 and quartz with thin-vein type from the characteristics of the deposit. The cause classification from different was is new and original in the paper. Its aim is to finding out the distribution regulation of the tungsten deposit and to serve for directing mine production and prospecting bitterly.
The 203 team of Changsha exploring company. the geology exploring summary report on Shang Ping tungsten mine in Yu Du county of Jiang Xi province[M]. Changsha: Changsha exploring company,1957. (In Chinese)
Gan Z, Zhong X. The Prediction of the deep exploring ores in mine in Shangping [J]. Metal Mine 2009; (11): 86-88. (In Chinese)
Jia M, Wang M, Li Y, Sun C. Characteristics of Chinese Tungsten Ore and the Problems in the Tungsten Resource Utilization [J]. Mining and Metallurgy 2013; (3): 90-94. (In Chinese)
Tan Y, Tong Q, Pi J, Deng G. Geological geochemical Features of Ore-near Hydrothermal Alteration Rocks in Pangushan Tungsten Deposit [J]. China Tungsten Industry 2002; (10): 21-26. (In Chinese)
Hua R, Chen P, Zhang W, Lu J. Three maj or metallogenic events in Mesozoic in South Chna [J]. Mineral Deposits 24(2): 99-105. (In Chinese).
Gan Z, Yang C. Causes Analysis of Tungsten Mine and Calculation of Ore Storage in Lei Gong Di [J]. Metal Mine 2009; (4): 84-86. (In Chinese)
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