THE PRELIMINARY STUDY OF FLUID INCLUSION CHARACTERISTICS IN SHIRENZHANG TUNGSTEN DEPOSIT, GUANGDONG PROVINCE, CHINA

摘要

The mineralization order of Shirenzhang tungsten is in accordance with "tungstate in first and sulfides in late". The metallogenic fluid is similar with Yaoling and Meiziwo deposits, which is the mixture of crust and mantle magmatic hydrotherm and transformational saturated atmospheric water and both belongs to W, Sn mineralization product in South China during the mid-massive.