Response of a mountain‐foreland fluvial system to an advancing ice sheet, southern Poland-Reference-Cited by-同舟云学术

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Response of a mountain‐foreland fluvial system to an advancing ice sheet, southern Poland

Published:2019-03-04 Issue:3 Volume:48 Page:695-712
ISSN:0300-9483
Container-title:Boreas
language:en
Short-container-title:Boreas

Author:

Salamon Tomasz¹^ORCID,Zieliński Tomasz²

Affiliation:

1. Department of Earth Science University of Silesia in Katowice Będzińska 60 Sosnowiec 41‐200 Poland

2. Faculty of Geographical and Geological Sciences Adam Mickiewicz University Krygowskiego 12 Poznań 61‐680 Poland

Funder

Narodowe Centrum Nauki

Publisher

Wiley

Subject

Geology,Archaeology,Ecology, Evolution, Behavior and Systematics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/bor.12389

Reference117 articles.

1. Environmental change and fluvial activity during the Younger Dryas in central Germany

2. Pleistocene fluvial terraces from northern France (Seine, Yonne, Somme): synthesis, and new results from interglacial deposits

3. How do gravel-bed rivers braid?

4. J. Badura B. Przybylski 1997

5. Extent of the Pleistocene Ice Sheets and deglaciation between the Sudeten and the Silesian Rampart;Badura J.;Biuletyn PIG,1998

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1. Sedimentary and structural record of the Scandinavian Ice Sheet margin dynamics at the SE part of the Głubczyce Plateau, a foreland of the East Sudetes Mountains (S Poland);Geomorphology;2022-09

2. Morphotectonic configuration of the Podtatranská Kotlina Basin and its relationship to the origin of the Western Carpathians;Geomorphology;2021-12

3. Ice-crevasse sedimentation in the eastern part of the Głubczyce Plateau (S Poland) during the final stage of the Drenthian Glaciation;Open Geosciences;2020-01-01

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