Mineralogical and geochemical peculiarities of the revealed graphite in ore veins of Kalgutinskii deposit are analyzed. The obtained data (Raman scattering, mass spectrometry, X-ray diffraction, coulometric titration - for analyzing carbon (organic) content and distribution in samples) indicate active participation of carbon in the ore formation process. Apparently, the plutonic metalliferous fluids having the reduced character were the carbon sources.
|Number of pages||4|
|Journal||Doklady Akademii Nauk|
|Publication status||Published - 2004|
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