Chemical composition of fluid inclusions in the ore
Chemical composition of oreforming minerals in antimony, mercury, mercuryarsenic and arsenic (realgar orpiment) deposits on the southern slope of the Great Caucasus has been investigated. These deposits represent medium and lowtemperature formations, developing stageby stage in quartzantimonite, quartzdickitecarbonatecinnabar and realgarorpiment stages of mineralization.