《Table 1 Mineral compositions of the ore body》

  提示：宽带有限、当前游客访问压缩模式

本系列图表出处文件名：随高清版一同展现

《"Mineralization, Geochemistry and Zircon U-Pb Ages of the Paodaoling Porphyry Gold Deposit in the Guichi Region, Lower Yangtze Metallogenic Belt, Eastern China"》

1. 获取 高清版本忘记账户？点击这里登录

1. 下载图表忘记账户？点击这里登录

Alteration and mineralization are widespread，mainly in the Paodaoling porphyry（Fig.5a–d），and partially developed in the Gaojiabian Formation（Fig.5f–g），including mainly sericitization，chloritization，silicification，carbonatization，muscovitization and kaolinization.Ore textures at Paodaoling are mainly massive，disseminated and veined（Fig.5）.The dominant ore minerals are pyrite，with a small amount of galena，sphalerite，chalcopyrite，magnetite，realgar and orpimentin the Paodaoling dacite porphyry and the surrounding Gaojiabian formation siltstone（Fig.5）.Gold does not exist as native Au，but in the form of ultramicroinclusions in sulfide minerals，mainly pyrite and arsenopyrite（Duan Liuan et al.，2014）.Supergene limonite and hematite caused by pyrite oxidation acted as the Au carrier in the oxidation zone on the surface.A complete list of ore mineral assemblages are shown in Table 1.Based on field ore deposit geology，hand specimen features，and microphotograph observation，the formation of the Paodaoling Au deposit can be roughly divided into three stages，i.e.，phyllic stage，poly-metal sulfide stage and supergene stage（Fig.7）: