| [1] |
1 刘立钧.387地注型古岩溶铀矿床成因探讨.铀矿地质.1985.1(6):1-10. 2 Shelton K L and Rye D M. Sulfur isotope compositions ofores from mines Cape, Quebec; an example of sulfate-sulfi deisotopic disequilibria in ore-forming fluids with applications to other porphyry-type deposits, Economic Geology, 198 77 1688-1709. 3 刘裕庆等.德兴斑岩铜(铝)矿田硫同位素地质特征初步研究.中国地质科学院1i).床地质研究所所刊(第1号)1982,58-65. 4 Sheppard S M F. Charackerization and isotopic variations in Ylatnral watersRev Mineralogy, 1986, 16 165- 183 5 ELSharkawi W A.ELArefM M and Motelib A AManganese deposits in a Carboniferous paleokarst profile, Um Bogma Region,West-central Sinal.Egypt, Mineralum De- posita, 1990, 25 34-43. 6 Olson RA. Genesis of paleoka rst and s t rat a-b ou nd zinc-leadsulfide deposits in a Proterozoic dolostonet NorthernIsland, Canada, Economic Geology, 1984, 79 1056-1103 7 W allace A R.The relief canyon gold deposit, Nevadaa mineralized solution breccia Economic Geology, 1989, 84 274-190 |