摘要
For the gold deposit in the metamorphic rock series of Tianzhu-Jinping-Liping area in southeast Guizhou Province,the metallogenic unit division and its ore-control factors are discussed.By field investigation and comprehensible study,the division of all gold belt and ore field are divided.Most of the divided gold field are controlled by NE anticlinorium and its secondary anticlinorium in Caledonian.Some is controlled by faulted block of both sides reverse fault of big anticlinorium,and some is controlled by EW fundamental fault and concealed terrain.