達城鑛山의 流體包有物에 依한 生成溫度와 鑛物共生에 關한 硏究

A study for genesis by homogenization temperature and paragenesis of Dalsung mine

Dalsung Mine, located in Kyungsang puk-do, Korea, is well known as one of the typical breccia pipe filling hydrothermal W-Cu deposit. By homogenization temperature with fluid inclusions in quartz crystals (330 samples were dealt with) by heating stage microscope, two temperature ranges were figured out one is 154°~267℃(average 210℃), and the other is 283°~335℃(average 309℃). Regarding to mineral paragenesis, mineralization of the deposit were thought that former, mesothermal stage, W-Cu mineralization processed through out the ore body and later mineralization were limitted under -4level as katathermal solution with Cu minerals.