摘要
The Shikebutai iron ore in Xinjiang is one afamous high-grad iron ore with long-mining time and high-grad at present.Through the study on silicate,REE and trace elements of ore body in mine rock,combined with site observation outdoor and microscopic analy indoor,this article discussed the metallogenic environment,mineral composition,source of ore-forming materials of the deposit deeply.and believed that genesis of ore deposit should be volcanic jet-hot water deposit type closely associated with the action of seawater in the undersea environment,having more detailed understanding of the metallogenic process,concretely dividing three stages: spray-flow deposits metallogenic,restore overflow hot water precipitation,enriched oxidation metallogenic.