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"Izuchenie sul'fidnykh vklyucheniy yavlyaetsya interesnoy zadachey, pozvolyayushchey detal'noe izuchenie usloviy obrazovaniya i preobrazovaniya vysokoorganicheskogo osadka. Sul'fidnye vklyucheniya predstavlyayut soboy chutkiy indikator usloviya osadkonakopleniya. Vse povyshennye kontsentratsii khimicheskikh elementov v sul'fidnykh vklyucheniyakh mogut byt' ob""yasneny mineral'nym sostavom neorganicheskoy chasti ugley. V kotoroy pomimo sul'fidnykh vklyucheniy prisutstvuet glinistoe veshchestvo (v osnovnom predstavlennoe kaolinitom), a terrigennaya sostavlyayushchaya predstavlena kvartsem, a takzhe v men'shem kolichestve rutilom, il'menitom, tsirkonom, baritom i dr. Po rezul'tatam provedennykh issledovaniy byli opredeleny veshchestvennyy (mineral'nyy i khimicheskiy) sostav ugley, ustanovleno, chem predstavleny sul'fidnye vklyucheniya i, kakie elementy v nikh preobladayut. Prisutstvuyushchie sul'fidy otrazhayut stadiynost' formirovaniya ugol'nogo plasta i izmenenie khimicheskogo sostava vod torfyanika. Geokhimicheskie osobennosti rasseyannykh elementov v sostave ugley svyazany s trudnorastvorimymi elementami-gidrolizatami (Ti, Zr, RZE)"

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