The Northern Pleistocene of Russia. [elektronicky zdroj]

Autor: Astakhov, Valery I.

Externí odkaz: Kolekce e-knih KNAV (Registrovani uzivatele: plny text online 5 minut, dalsi pristup na vyzadani. Registered users: full text online 5 minutes, further access on requests.)

Glacial and vegetation history of the Polar Ural Mountains in northern Russia during the Last Ice Age, Marine Isotope Stages 5–2

Autor: Svendsen, John Inge, Krüger, Linn Cecilie, Mangerud, Jan, Astakhov, Valery I., Paus, Aage, Nazarov, Dmitry, Murray, Andrew

Publikováno v: In Quaternary Science Reviews 15 May 2014 92:409-428

The periglacial climate and environment in northern Eurasia during the Last Glaciation

Autor: Hubberten, Hans W ^*, Andreev, Andrei, Astakhov, Valery I, Demidov, Igor, Dowdeswell, Julian A, Henriksen, Mona, Hjort, Christian, Houmark-Nielsen, Michael, Jakobsson, Martin, Kuzmina, Svetlana, Larsen, Eiliv, Lunkka, Juha Pekka, Lyså, Astrid, Mangerud, Jan, Möller, Per, Saarnisto, Matti, Schirrmeister, Lutz, Sher, Andrei V, Siegert, Christine, Siegert, Martin J, Svendsen, John Inge

Publikováno v: In Quaternary Science Reviews 2004 23(11):1333-1357

The chronology of a large ice-dammed lake and the Barents–Kara Ice Sheet advances, Northern Russia

Autor: Mangerud, Jan ^*, Astakhov, Valery I, Murray, Andrew, Svendsen, John Inge

Publikováno v: In Global and Planetary Change 2001 31(1):321-336

Age and extent of the Barents and Kara ice sheets in Northern Russia

Autor: Mangerud, Jan, Svendsen, John Inge, Astakhov, Valery I., Andreicheva, Ludmila, Funder, Svend, Henriksen, Mona, Hufthammer, Anne Karin, Indrelid, Svein, Matiouchkov, Alexei, Murray, Andrew, Paus, Aage, Pavlov, Pavel, Tveranger, Jan, Ulvedal, Per

Publikováno v: Mangerud, J, Svendsen, J I, Astakhov, V I, Andreicheva, L, Funder, S, Henriksen, M, Hufthammer, A K, Indrelid, S, Matiouchkov, A, Murray, A, Paus, A, Pavlov, P, Tveranger, J & Ulvedal, P 1999, ' Age and extent of the Barents and Kara ice sheets in Northern Russia ', Boreas, vol. 28, no. 1, pp. 46-80 . https://doi.org/10.1111/j.1502-3885.1999.tb00206.x

The youngest ice marginal zone between the White Sea and the Ural mountains is the W-E trending belt of moraines called the Varsh-Indiga-Markhida-Harbei-Halmer-Sopkay, here calledthe Markhida line. Glacial elements show that it was deposited by the K

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b06b6b75a011cde891d6fd12ba633a00
https://doi.org/10.1111/j.1502-3885.1999.tb00206.x