han; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto" class=MsoNormal>In hemas-microsoft-com:office:smarttags" />Southeast Guizhou Province, primary gold mineralization in the turbidites hosted by the Presinian Xiajing Group (meta-slate, sandstone and meta-tuff) is associated with quartz veins. The gold deposits all occurred at the NE-fold axis. Ore-forming materials were activated, transported and enriched during deformation and finally concordant and discordant gold-bearing quartz-veins were formed. The experimental results are consistent well with the characteristics of the quartz-vein gold deposits in the area studied. It will provide scientific experimental data and useful information about ore-forming rules and ore prognosis. hemas-microsoft-com:office:office" />