The Sain Us gold deposit is a typical auriferous sulfide quartz vein deposit in the arid grassland climatic zone of Inner Mongolia The oxidation zone has been controlled by the arid climate since the beginning of Holocene. Gold supergene evolution is char
马民涛,关广岳.1996.内蒙古干旱区赛乌素金矿氧化带及金表生地球化学研究[J].地质学报,70(3). Ma Mintao.1996. SUPERGENE GEOCHEMISTRY OF GOLD AND OXIFATION ZONE OF THE SAIN US GOLD DEPOSIT OF THE INNER MONGOLIA ARID CLIMATIC REGION[J]. Acta Geologica Sinica,70(3).
