NEW DATA ON ISOTOPIC COMPOSITION OF HYDROTHERMAL OIL FROM THE UZON CALDERA, KAMCHATKA

dc.contributor.author	Lukin A.E.
dc.contributor.author	Pikovskii Yu.I.
dc.date.accessioned	2022-08-14T03:31:08Z
dc.date.available	2022-08-14T03:31:08Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=13470617
dc.identifier.citation	Doklady Earth Sciences, 2004, 398, 7, 931-934
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/38525
dc.description.abstract	The hydrothermal oil in the Uzon caldera is represented by two fractions (generations) separated in time and, partially, in space. The first generation is observed as green (rapidly turning brown in air) heavy (0.9148-0.9767 g/cm3) viscous and resinous (up to 9.3% of resin), sulfurous (up to 2%), low-paraffin (up to 2.1%) oil of the methane-naphthene-aromatic type with a uniquely high optic activity (αD = 24.2%) and extremely low degree of maturity. The second generation makes up colorless hydrocarbon condensate (with a strong kerosene smell) that rapidly spreads as iridescent films and gradually evaporates. This condensate is close to the low-density light-colored naphtha from the Bogachev field.
dc.title	NEW DATA ON ISOTOPIC COMPOSITION OF HYDROTHERMAL OIL FROM THE UZON CALDERA, KAMCHATKA
dc.type	Статья

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