L. V. Alabin. GEOLOGY AND GEOCHEMISTRY OF GOLD DEPOSITS IN THE SOUTHWEST OF SIBERIAN PLATFORM[J]. Geology and Resources, 1993, 2(1): 1-8. DOI: 10.13686/j.cnki.dzyzy.1993.01.001
    Citation: L. V. Alabin. GEOLOGY AND GEOCHEMISTRY OF GOLD DEPOSITS IN THE SOUTHWEST OF SIBERIAN PLATFORM[J]. Geology and Resources, 1993, 2(1): 1-8. DOI: 10.13686/j.cnki.dzyzy.1993.01.001

    GEOLOGY AND GEOCHEMISTRY OF GOLD DEPOSITS IN THE SOUTHWEST OF SIBERIAN PLATFORM

    • There are two kinds of gold-deposit formations within Caledonian foldsystem in the southwest of Siberian platform:a. Gold-sulfide-quartz forma tion; b. Gold-skarn forma tion. They are formed in geodynamic tectonic surroundings of ancient island arc, usually occured in the zone of ophiolitic formation and related with proto -plutonic granitoid rocks in genesis. Associated elements of the ore, Cu, Pb and Zn, are 10-20 times as much as that of wall rocks. As, Sb, Mo, W, Bi and Te etc. may act as indicator for industrial orebody.
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