///Yemaquan gold deposit is located at axis of Hasafen anticlinorium in the west side of the big Kasikaiersuokekan fault belt in south part of Late Paleozoic continent marginal basin in the east Zubger area of the micro-Zubger plate. Ore bodies occur in the altered diorite dykes or at their inner and outer contact zones. The altered diorite dykes are enclosed in argillaceous slate and phyllitized siltstone of the Lower Silurian Kubusu group. Genetically, the gold deposit is a sub-volcanic-metamorphic hydrothermal deposit.