与低O岩浆有关的矽卡岩型铅锌矿床

[1] 岩浆成因夕卡岩的包裹体证据[J] 赵斌，李院生，赵劲松 地球化学 1995, 02

[2] Trace elements (REE) and isotopes (O; C; Sr) to characterize the metasomatic fluid sources: evidence from the skarn deposit (Fe; W; Cu) of Traversella (Ivrea; Italy)[J] J. Auwera;L. Andre Contributions to Mineralogy and Petrology 1991,

[3] Stable isotope studies of metasomatic Ca-Fe-Al-Si skarns and associated metamorphic and igneous rocks; Osgood Mountains; Nevada[J] Bruce E. Taylor;James R. O'Neil Contributions To Mineralogy And Petrology 1977,

[4] 稳定同位素在地质科学中的应用[M] 张理刚著; 陕西科学技术出版社 1985,

[1] 岩浆成因夕卡岩的包裹体证据[J] 赵斌，李院生，赵劲松 地球化学 1995, 02

[2] Trace elements (REE) and isotopes (O; C; Sr) to characterize the metasomatic fluid sources: evidence from the skarn deposit (Fe; W; Cu) of Traversella (Ivrea; Italy)[J] J. Auwera;L. Andre Contributions to Mineralogy and Petrology 1991,

[3] Stable isotope studies of metasomatic Ca-Fe-Al-Si skarns and associated metamorphic and igneous rocks; Osgood Mountains; Nevada[J] Bruce E. Taylor;James R. O'Neil Contributions To Mineralogy And Petrology 1977,

[4] 稳定同位素在地质科学中的应用[M] 张理刚著; 陕西科学技术出版社 1985,