Nn. Baranova et al., CONTENTS AND CHEMICAL FORMS OF AU, TE, SB AND AS IN MINERAL-FORMING SOLUTIONS GOLD-SULFIDE-TELLURIDE EPITHERMAL DEPOSITS - ON FLUID INCLUSIONS DATA, Geohimia, (12), 1995, pp. 1786-1799
Fluid inclusions in quartz samples taken as representative in respect
of main mineral assemblages of three gold-sulfide/telluride epithermal
ore deposits were studied. Gold, arsenic, antimony and tellurium cont
ent were determined by use of neutron activation and atomic absorption
analysis, the corresponding values being as following: 10(-6)-10(-4,5
), 10(-2,5),-10(-1,2), 10(-2,2)-10(-0,5), 10(-6)-10(-4) M. The complex
ions Au(HS)(2)(-), H3AsO30, HSb2S4- and HTe-were found as predominant
chemical forms of Au, As, Sb and Te in ore forming solutions, Covaria
tive character of gold distribution in relation to that of arsenic and
antimony in fluid inclusions is interpreted as indicative of the prob
able gold transport in the form of sulfur-bearing complex compounds wi
th arsenic and/or antimony in the sulfide oreforming processes. The re
ciprocal correlation of gold and tellurium content could be considered
as an evidence of Te ore-concentrator role in the Au-Te mineralisatio
n.