- 责任者：Sun He (Key Laboratory of Mineral Resources ; Institute of Geology and Geophysics ; Chinese Academy of Sciences ; Beijing 100029 ; China) ; Tang Dongmei
- 刊名：Geological Review
- 出版年：2009
- 卷期：55(6)
- 关键词：亲铜元素 ; chalcophile elements ; 块状流化物矿床 ; massive sulfide deposits
- 页码：p.840-850
- 图表：4 illus., 1 table, 78 refs.
- 分类号：0600
- issnNo：ISSN0371-5736
- isbnNo：CN11-1952/P
///This paper summarizes the behavior of sulfur and chalcophile elements in magma evolution, and demonstrates their application in the study of magmatic sulfide deposits. They are discussed from five factors: 1) by the study of sulfur solubility in basaltic magma, four factors control the sulfide segregation: magma mixing, rapid temperature decrease, crustal contamination, and rapid crystal fractionation; 2) according to the distribution of Ni between olivine and silicate magma, we simulate the correlated change of Ni in olivine to Fo; 3) the D values of Ni—Cu and PGE between sulfide liquid and silicate melt is are summarized, and the controlling factors to D value and R-factor are discussed also; 4) when olivine is surrounded by sulfide liquid, the interaction will happen, and Ni content in sulfide liquid can be estimated; and 5) by the distribution of chalcophile elements between MSS and sulfide liquid, the facts of ore-forming zonations are summarized. At the end, the present problems and direction of development are analyzed and suggested.