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dc.contributor.author Ganzei L.A.
dc.contributor.author Razzhigaeva N.G.
dc.date.accessioned 2024-12-22T03:48:06Z
dc.date.available 2024-12-22T03:48:06Z
dc.date.issued 2006
dc.identifier https://www.elibrary.ru/item.asp?id=13529844
dc.identifier.citation Lithology and Mineral Resources, 2006, 41, 3, 215-221
dc.identifier.issn 0024-4902
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/47107
dc.description.abstract Lithostructural composition of the dust storm material (DMS) sampled in the southern Far East in the spring of 2002-2004 has been analyzed. Samples were taken near Vladivostok, where the eolian dust precipitation varied from 0.1 to 6.5 g/m2 at that time. Pelitic and fine-silt particles predominate in eolian dust. Grain size, mineral, and chemical compositions of the DSM are compared to data on the DSM in adjacent territories of China, Korea, and Japan, as well as to background data on aerosol precipitation in southern Primorye. Possible mechanisms of the eolian dust transport from inner parts of Asia at different climatic variations in the Pleistocene-Holocene are discussed. © Pleiades Publishing, Inc. 2006.
dc.subject Holocene
dc.subject Pleistocene
dc.title COMPOSITION OF SAND STORM PARTICLES IN THE SOUTHERN FAR EAST
dc.type Статья
dc.identifier.doi 10.1134/S0024490206030023
dc.subject.age Cenozoic::Quaternary::Holocene
dc.subject.age Кайнозой::Четвертичная::Голоцен
dc.subject.age Cenozoic::Quaternary::Pleistocene
dc.subject.age Кайнозой::Четвертичная::Плейстоцен


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