Fineness, Trace Elements and the Internal Structure of the Dagkhasaman Native Gold Deposit (Lesser Caucasus)
This article considers fineness, trace elements and the internal structure of native gold of Dagkesaman field. As a r esults of analysis of monomineralic fractions of sulfide minerals found that the major gold-bearings in this field are sphalerite, galena and partially chalcopyrite. It is established that, Dagkesaman polymetallic gold deposits formed in shallow conditions. The study found that the gold fineness varies over a wide range (from 800 to 950 ‰), trace elements (Cu, Fe, Pb, Zn, Te, Bi, Mo, As) is determined and revealed the following internal structure: homogeneous, zonal, mono-granular, spotty, which have great practical significance in determine genesis of the deposits and their prediction and assessment of the present work.