ISOTOPIC SIGNATURES OF DEPOSITION AND TRANSFORMATION OF LOWER CAMBRIAN SALIFEROUS ROCKS IN THE IRKUTSK AMPHITHEATER: COMMUNICATION 1. SULFUR ISOTOPIC COMPOSITION

Простая страница элемента
dc.contributor.authorVinogradov V.I.
dc.contributor.authorBujakaite M.I.
dc.contributor.authorKuleshov V.N.
dc.contributor.authorPokrovskii B.G.
dc.contributor.authorBelenitskaya G.A.
dc.contributor.authorMinaeva M.A.
dc.date.accessioned2024-12-15T02:15:23Z
dc.date.available2024-12-15T02:15:23Z
dc.date.issued2006
dc.description.abstractNew isotope data on Lower Cambrian rocks of the Irkutsk amphitheater are reported in three communications. The first communication is devoted to the sulfur isotopic composition, which is most sensitive to ostsedimentary geochemical transformations of sulfate rocks in saliferous formations. It is shown that δ34S values in Bel'sk and Zhigalovo boreholes are within 22-35‰ The lowest values are close to the sulfur isotopic composition of a halogenic basin, while the highest values are related to epigenetic sulfate reduction. This process was responsible for the elimination of 100 m of anhydrites from the Lower Cambrian section. © Pleiades Publishing, Inc. 2006.
dc.identifierhttps://www.elibrary.ru/item.asp?id=13511214
dc.identifier.citationLithology and Mineral Resources, 2006, 41, 1, 85-97
dc.identifier.doi10.1134/S002449020601007X
dc.identifier.issn0024-4902
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/47011
dc.subjectCambrian
dc.subject.agePaleozoic::Cambrian
dc.subject.ageПалеозой::Кембрийская
dc.titleISOTOPIC SIGNATURES OF DEPOSITION AND TRANSFORMATION OF LOWER CAMBRIAN SALIFEROUS ROCKS IN THE IRKUTSK AMPHITHEATER: COMMUNICATION 1. SULFUR ISOTOPIC COMPOSITION
dc.typeСтатья

Файлы

Оригинальный пакет

Показано 1 - 1 из 1
Изображение-миниатюра
Имя:
Vino_06.pdf
Размер:
196.73 KB
Формат:
Adobe Portable Document Format
Скачать

Коллекции

ELibrary