Economic and Environmental Geology (자원환경지질)
- Volume 12 Issue 4
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- Pages.197-206
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- 1979
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- 1225-7281(pISSN)
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- 2288-7962(eISSN)
Fluid Inclusion Study of Sangdong Tungsten Deposits
상동(上東) 중석광상(重石鑛床)의 유체포유물(流體包有物) 연구(硏究)
Abstract
Sangdong scheelite deposit is confirmed to have been formed by replacement of limestone beds by metasomatic mineralization. Mineralogical zonal distribution and filling temperatures are related with order of its formation and tungsten mineralization. The first formed garnet-pyroxene zone, left in the margins of the ore body, shows the highest filling temperature of fluid inclusions in pyroxene, averaging
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