摘要
The Pingshui copper deposit is the biggest copper deposit in Zhejiang Province, and is a typical massive sulfide deposit in the northeast part of Qinzhou-Hangzhou collision belt between Yangtze and Cathaysia blocks. This paper made systematic research works on fluid inclusions in Pingshui copper deposit. The type of fluid inclusions is very sample, mainly the liquid (H2O)-rich inclusions. The identification of fluid verified the causation of Pingshui copper deposit, that it belongs to a typical volcanic-hosted massive sulfide deposit. The results are of great significance for further researches on the genesis, formation and evolution of the Pingshui copper deposit.