SUMMARY
It was found that native sulphur of indUllltrial
frii ..
portance, for IWhichas"-
+l1l1fto,
is accompanied by limestones, for which 8CJI - -dO"'. In turn,~u1phJll" characterized by lower values, i.e.as" -
0, IOCcurrhig at the periphery of the sulpbur ore, is accompanied . by limestones, for which 8ClS - -20%0. Thus it is :Inferred thatt Itbe sulphur of industrial im~ce was furmed in result of illltensive gypsum re"tiction processes under the influence of methane, whereas peripheral sulphur !WaS formed in results of slowerreduction processes under the influence of .h~er oil fractions.
B paC50Te ODHC8H8 m.uumeHHaH 38KOHOMepHOCT&, COC'ro~8H B TOll, 'IT'O caMOPO~R8H cepa npoMhlIlIneH-Horo co~eplKaRKIl c b"S - +101lM CODpoBolK~a~.JJ .
HS-BecTHHKaMH, B KOTOPhIX 813C - -10%0. Cepa c
HH3KH-MK CO;tteplKaRHHMH 834S - 0, pacnpoCTpRHeHHaH B
ne-pHCi>ePH'ieCK'Clilt 'laCTH sanelKH, conpoBO)K~aeTCH
HS-Be~ . C . lI13C'--201lM •. 3To MOlKlIO 06'hHCHHTh
TIlKHK ofipasoM, '{TO cepa npOMJ>OUneHSOro TKIIa
oOpa-3OBU8e& B pesym.T8Te HHTeHCHBHOro BOCCTaHOBmeHHH
rHlICos .. ~ .BJIJUliIKeK KeTaBa, cepa. lKe
nepU<PePH-'leCKoA -!3OHhI - B more Me~neHHoro BOCCTaHOBneHHH