Osobennosti krupnoob#emnyh mestorozhdenij zolota

Awtor wydelqet specificheskie osobennosti osnownyh swojstw mestorozhdenij zolota, swqzannyh s "chernoslancewymi" tolschami- regional'noe rasprostranenie zolotonosnoj formacii, stadijnost' rudoobrazowaniq w hode diageneza metamorfizma i postmagmaticheskogo preobrazowaniq. Awtor obosnowywaet celesoobraznost' ih ob#edineniq w ob#emnuü rudno-magmaticheskuü sistemu, dlq kotoroj harakteren bol'shoj masshtab rudonosnosti. Vse äto harakterizuet rudonosnuü sistemu kak weduschuü mineral'no-syr'ewuü bazu zolotodobychi. V osobennosti, esli prinqt' wo wnimanie swqz' s rajonami razwitiq chernoslancewogo komplexa mestorozhdenij osnownyh rossypej zolota. The author highlights the specific characteristics of the basic properties of gold deposits,connected with black shales-regional distribution of stages of formation of the gold ore, formation during metamorphism diagenez and postmagmatism conversion. These features are associated with black shales- layers. The author proves the usefulness of combining them into larger ore-magmatism system, characterized by a large scale of ore-bearing potential. All this defines ore-bearing system as the leading mineral resources potential of gold mining. Especially if you t