New Insights on the Formation of Magmatic Sulfide Deposits in Magma Conduit System

• 责任者：Song Xieyan (State Key Laboratory of Ore Deposit Geochemistry ; Institute of Geochemistry ; Chinese Academy of Sciences ; Guiyang 550002 ; China) ; Xiao Jiafei
• 刊名：Earth Science Frontiers
• 出版年：2010
• 卷期：17（1)
• 关键词：硫化物矿床 ; sulfide deposit ; 岩浆作用 ; igneous activity
• 页码：p.153-163
• 图表：4 illus., 1 tables, 35 refs.
• 分类号：1001
• issnNo：ISSN1005-2321
• isbnNo：CN11-3370/P

The three most important elementary factors for the formation of large-super large magmatic sulfide deposits are that 1) large amount of mantle-derived magmas participate in the formation of the deposits, that 2) magmatic evolution results in sulfide immiscibility, and that 3) the sulfides concentrate in a limited space. In this paper, the authors attempt to demonstrate the general features, formation mechanism and geological background, and significance of the magmatic sulfide deposits occurring in magmatic conduit system, which are very important for the further researches and exploration of this type of magmatic sulfide deposits.