期刊文献+

Complexation of Si in Hydrothermal Systems

Complexation of Si in Hydrothermal Systems
下载PDF
导出
摘要 The Au\|SiO\-2 and Sn\|SiO\-2 complexes have been experimentally calibrated at varying temperature, silica concentration and pH: Au\+++H\-3SiO\+-\-4AuH\-3SiO\-4lgK=-1.65436+9611.21/T Sn\+\{4+\}+4H\-3SiO\+-\-4Sn(H\-3SiO\-4)\-4lgK\-\{200℃\}=42.73Compared with Au\|Cl, Au\|HS and Sn\|OH complexes, AuH\-3SiO\-4 and Sn(H\-3SiO\-4)\-4 complexes can be recognized as the dominant transport forms in Si\|bearing solutions under pH and Eh conditions of general interest. The decrease of SiO\-2 concentration and oxygen fugacity would reverse the direction of dissolution\|complexing reactions, resulting in the precipitation of gold and silica, as well as cassiterite and silica. This study illustrates the significance of SiO\-2\|complexation in hydrothermal solutions for gold, tin and other metallizations. The Au\|SiO\-2 and Sn\|SiO\-2 complexes have been experimentally calibrated at varying temperature, silica concentration and pH: Au\+++H\-3SiO\+-\-4AuH\-3SiO\-4lgK=-1.65436+9611.21/T Sn\+\{4+\}+4H\-3SiO\+-\-4Sn(H\-3SiO\-4)\-4lgK\-\{200℃\}=42.73Compared with Au\|Cl, Au\|HS and Sn\|OH complexes, AuH\-3SiO\-4 and Sn(H\-3SiO\-4)\-4 complexes can be recognized as the dominant transport forms in Si\|bearing solutions under pH and Eh conditions of general interest. The decrease of SiO\-2 concentration and oxygen fugacity would reverse the direction of dissolution\|complexing reactions, resulting in the precipitation of gold and silica, as well as cassiterite and silica. This study illustrates the significance of SiO\-2\|complexation in hydrothermal solutions for gold, tin and other metallizations.
出处 《Chinese Journal Of Geochemistry》 EI CAS 2001年第3期201-209,共9页 中国地球化学学报
基金 ThisresearchprojectwasgrantedjointlybytheNationalNaturalScienceFoundationofChina (GrantNo .49373181)andtheOpenLab .ofOreDeposi
关键词 金矿化作用 硅化作用 硅酸 水岩反应 gold\|silica complexation tin\|silica complexation transport form silicification gold mineralization
  • 相关文献

参考文献9

  • 1[1]Chou, I.M., 1989, A low-temperature redox sensor: EOS, v.70, n. 15, p.507. 被引量:1
  • 2[2]Dadze, T.P., V.I. Sorokhin, and I. Y. Nekrasov, 1982, Solubility of SnO2 in water and in aqueous solutions of HCl, HCl + KCl and HNO3 at 200 - 400 ℃ and 101.3 MPa: Geochem. Int., v. 19, p. 142 - 152. 被引量:1
  • 3[3]Fan Wenling, Wang Shengyuan, and Wu Jianjun, 1993, Experimental calibration of Au-Si complexation in low temperature hydrothermal solutions: Chinese Science Bulletin, v. 38, n. 10, p. 933- 935. 被引量:1
  • 4[4]Fan Wenling, Wang Shengyuan, and Tian Yifu, 1997, Experimental study on the complexation of SiO2 with the ore-forming element Sb.. Acta Mineralogica Sinica, v. 17, n. 4, p. 472- 477 (in Chinese with English ab stract). 被引量:1
  • 5[5]Henley, R.W., 1984, pH calculations of hydrothermal fluids, in fluid-mineral equilibria in hydrothermal systems(Chapter 7): Reviews in Ecom. Geol., n. 1, p. 90. 被引量:1
  • 6[6]Helgeson, H.C., 1969, Thermodynamics of hydrothermal systems at elevated temperatures and pressures: Amer.J. Sci., v. 267, p. 729 - 804. 被引量:1
  • 7[7]Huston, D.L. and R.A. Largers, 1989, Chemical model for the concentration of gold in volcanogenic massive sul fide deposits: Ore Geology Reviews, n. 4, p.171- 200. 被引量:1
  • 8[8]Jzckson, K.J. and H.C. Helgeson, 1985, Chemical and thermodynamic constraints on the hydrothermal transport and deposition of tin: I. Calculation of the solubility of cassiterite at high pressures and temperatures:Geochim. et Cosmochim. Acta, v.49, p. 1 - 22. 被引量:1
  • 9[9]Wood, S.A., D.A. Crerar, and M.P. Boresik, 1987, Solubility of the assemblage pyrite-magnetite-sphalerite galena-gold-stibnite-bismuthinite-argentite-molybdenite in H2O-NaCl-CO2 solutions from 200℃ to 350℃: E con. Geol., v.82, p. 1864-1887. 被引量:1

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部