The aim of this paper is to discuss the later changes of hatu gold deposit.The author found that the quartz-vein type orebody is intimately related with granitic magma.It's the product that the non-mineralized fluid of granitic magma superimposed on the early altered rock type orebodies.The tectonic reconstruction has a little influence on the changes of the orebodies.The upper part of some quartz-vein type orebodies may be disappeared due to weathering denudation.This study find that the later reform actions have a great influence on the preservation of orebody.We must pay more attention to the altered rock type orebodies hidden under the quartz-vein type orebodies.