The Liushanyan copper- zinc deposit lies in the layer of laminated siliceous albitite．The ore shows laminarand prim ary brecciated textures． From the center to the margin of the orebodies there shows a comparativemineral zonation of pyrite- chalcopyrite- galena- barite- quartz． The concentration and component zonationof anomalies shows the duration and changes of mineralization within a certain geological time domain．Thesam e component zonation is seen in the horizontal and axial directions，and from the center to the m argin，itshows a zonation of Cd— Ge— Bi— As— Ga— Cu— M o— Zn— Pb— Ag— Ba— M n— V— W ． According to theassemblage，intensity and ratio of the anom aly elements the denudation degree of orebodies can be determined．The most important is that stream sediments of the host rocks of the massive sulfide deposit have an extremelyhigh dilution rate under humid and hot conditions．M aking best use of the subm arine thermal water eruptionfacies m odel and outlining weak and local geochemical anomalies are the fundam ental means in geologicalexploration