Self‐constraining of low‐energy rivers explains low channel mobility and tortuous planforms-Reference-Cited by-同舟云学术

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Self‐constraining of low‐energy rivers explains low channel mobility and tortuous planforms

Published:2020-05-19 Issue:3 Volume:6 Page:648-669
ISSN:2055-4877
Container-title:The Depositional Record
language:en
Short-container-title:Depositional Rec.

Author:

Candel Jasper H. J.¹^ORCID,Makaske Bart¹,Kijm Niels¹,Kleinhans Maarten G.²,Storms Joep E. A.³^ORCID,Wallinga Jakob¹

Affiliation:

1. Soil Geography and Landscape Group Wageningen University and Research Wageningen The Netherlands

2. Department of Physical Geography Faculty of Geosciences Utrecht University Utrecht The Netherlands

3. Faculty of Civil Engineering and Geosciences Delft University of Technology Delft The Netherlands

Funder

Nederlandse Organisatie voor Wetenschappelijk Onderzoek

Publisher

Wiley

Subject

Paleontology,Stratigraphy,Geology,Environmental Science (miscellaneous),Oceanography

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/dep2.112

Reference98 articles.

1. The role of soil in vegetated gravelly river braid plains: more than just a passive response?

2. Late Weichselian and Holocene palaeogeography of the Rhine–Meuse delta, The Netherlands

3. Berendsen H.J.andStouthamer E.(2001)Palaeogeographic development of the Rhine‐Meuse delta the Netherlands Koninklijke van Gorcum.Assen.268Pages.

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