The last Fennoscandian Ice Sheet glaciation on the Kola Peninsula and Russian Lapland (Part 1): Ice flow configuration-Reference-Cited by-同舟云学术

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The last Fennoscandian Ice Sheet glaciation on the Kola Peninsula and Russian Lapland (Part 1): Ice flow configuration

Published:2023-01 Issue: Volume:300 Page:107871
ISSN:0277-3791
Container-title:Quaternary Science Reviews
language:en
Short-container-title:Quaternary Science Reviews

Author:

Boyes Benjamin M.^ORCID,Linch Lorna D.,Pearce Danni M.,Nash David J.^ORCID

Funder

University of Brighton

Publisher

Elsevier BV

Subject

Geology,Archeology,Archeology,Ecology, Evolution, Behavior and Systematics,Global and Planetary Change

Reference71 articles.

1. Études sur les Glaciers;Agassiz,1840

2. The deglaciation of Norway 15,000-10,000 BP;Andersen;Boreas,1979

3. The Younger Dryas margin of the Scandinavian Ice Sheet - an introduction;Andersen;Quat. Int.,1995

4. Stratigraphy. Murmansk region, Karelia, west of Arkhangelsk Region, NW of Vologda region and north of Leningrad Region;Apukhtin,1967

5. History of geological development of NW European part of USSR in Quaternary time;Apukhtin,1967

Cited by 2 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. Younger Dryas and Early Holocene ice‐margin dynamics in northwest Russia;Boreas;2024-03-03

2. Glacial geomorphology of the Republic of Karelia, northwest Russia: the Younger Dryas-early Holocene ice marginal zone;Journal of Maps;2023-07-07

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