Paper No. 0
Presentation Time: 4:00 PM
RETROGRADE AG-ENRICHMENT IN FAHLORES FROM THE COEUR D'ALENE MINING DISTRICT
Microprobe analyses, corona textures, massbalance constraints and mineral assemblages in sulfide ores from the Coeur dAlene mining district (Idaho) demonstrate that tetrahedrite fahlores [~ (Cu,Ag)10(Zn,Fe)2Sb4S13] in these ores have been enriched in Ag by the AgCu exchange reaction
0.1 Cu10(Zn,Fe)2Sb4S13 + AgSbS2 + PbS=CuPbSbS3 + 0.1 Ag10(Zn,Fe)2Sb4S13
which occurred during cooling following galena mineralization. This solidstate reaction resulted in quantitative removal of Ag from galena and can account for all of the bournonite mineralization. In galenarich samples it resulted in the highest Ag tetrahedrite fahlores found in the district. Fahlore molar Ag/(Ag+Cu)=0.303±0.011 and 0.336±0.011 were found in samples which achieved saturation with respect to other Agsulfosalts, namely pyrargyrite [~ Ag3SbS3] and polybasite [~ (Ag,Cu)16Sb2S11] in the West Chance and diaphorite [~ Pb2Ag3Sb3S8] in the Gold Hunter vein systems, respectively. This solidstate reaction may explain why previous district studies have been unable to convincingly demonstrate primary fahlore zoning. Based on thermodynamic analysis of Ag nettransport reactions involving Ag10Zn2Sb4S13 and other Agsulfosalts and the FeZn exchange reaction between fahlore and sphalerite, it is estimated that these reactions ceased below about 175°C. From a comparison of the results of this thermodynamic analysis with composition data for other Ag tetrahedrite fahlores found in the Coeur dAlene district and elsewhere, we conclude that the thermodynamic mixing properties of (Cu,Ag)10(Zn,Fe)2Sb4S13 fahlores are adequately characterized, but that further study of those of Ferich sphalerites are warranted.