New Data on Minerals. 2014. Vol. 49 57 NEW DATA ON MINERALOGY OF DEPOSITS OF PLUTONOGENIC GOLD-QUARTZ FORMATION IN THE NORTHERN CENTRAL KAZAKHSTAN. PART I Ernst M. Spiridonov Moscow State University, Geological Faculty, Moscow,
[email protected] The formation history of mineralogy of plutonogenic gold-quartz deposits of the Stepnyak group in the Northern Central Kazakhstan is discussed. Mineral facies referred to the depth of the deposit formation; mi ne - ralogical features of ore shoots, nature of ore-bearing fluids, white micas, quartz, carbonates, scheelite, pyrite, arsenopyrite, pyrrhotite, gersdorffite, sphalerite, berthierite, argentotennantite, argentotetrahedrite, roshchi- nite, bismuth tellurides and sulfotellurides, mattagamite, Co-bearing frohbergite and melonite, montbrayite, calaverite, sylvanite, petzite, petzite-hessite solid solution, and hessite are reported. The deposition sequence from Au to Ag tellurides and affinity for Te: Co > Fe, Ni > Bi, Sb > Pb > Ag, Hg > Au, Cu are improved. 10 figures, 8 tables, 60 references. Keywords: scheelite, mattagamite, frohbergite, melonite, montbrayite, calaverite, krennerite, sylvanite, pet- zite-hessite solid solution, affinity to Te. Despite many reviews, current state of geo - diately predated or accompanied gold minera- logy causes genetic typification of gold de - lization. posits. One of the ways is the detailed study of Plutonogenic hydrothermal gold-quartz specific gold formations, and separate gold formation. The deposits of the plutonogenic provinces and deposits. gold-quartz beresite-listvenite formation are Hydrothermal gold deposits are frequently paragenetically related to tonalite-grano dio rite- referred to the three formations on the basis of plagiogranite, adamellite, and monzo nite-gra- the formating depth: (1) shallow (with abun- nite intrusive complexes of folded areas.