H2S-bearing inclusions in recrystallized halite

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dc.contributor.author Grishina S.N.
dc.date.accessioned 2020-04-13T10:52:10Z
dc.date.available 2020-04-13T10:52:10Z
dc.date.issued 1987
dc.identifier https://elibrary.ru/item.asp?id=30969397
dc.identifier.citation CHEMICAL GEOLOGY, 1987, 61, 1-4, 91-94
dc.identifier.issn 0009-2541
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/16708
dc.description.abstract On a cryogenic investigation solid H2S was successively observed after freezing CO2 in water-poor fluid inclusions in halite of Cambrian Siberian salts. Melting of a H2S solid phase occurs at nearly eutectic temperatures of −95.6°C in CO2-H2S inclusions and in the range −98° to −100°C in CO2-H2S-CH4 or CO2-H2S-N2 inclusions. The compositions of the inclusions were determined by Raman microspectrometry.
dc.subject Cambrian en
dc.title H2S-bearing inclusions in recrystallized halite
dc.type Статья
dc.subject.age Paleozoic::Cambrian en
dc.subject.age Палеозой::Кембрийская ru


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