Response of the Rhine-Meuse fluvial system to Saalian ice-sheet dynamics

F.S. Busschers; R.T. van Balen; K.M. Cohen; C. Kasse; H.J.T. Weerts; J. Wallinga; F.P.M. Bunnik

doi:10.1111/j.1502-3885.2008.00025.x

Response of the Rhine-Meuse fluvial system to Saalian ice-sheet dynamics

F.S. Busschers
, R.T. van Balen
, K.M. Cohen
, C. Kasse
, H.J.T. Weerts
, J. Wallinga
, F.P.M. Bunnik

Dept of Biology

extern

Research output: Contribution to journal › Article › Academic › peer-review

Original language	English
Pages (from-to)	377-398
Number of pages	22
Journal	Boreas
Volume	37
DOIs	https://doi.org/10.1111/j.1502-3885.2008.00025.x
Publication status	Published - 2008

Access to Document

10.1111/j.1502-3885.2008.00025.xLicence: Unspecified

137 Citations
1 Meeting Abstract

The successive roles of proglacial drainage, normal ice-age rivers and marine processes in eroding the Strait of Dover and adjacent southernmost North Sea in the last 500 ka
Cohen, K. M., 2012, In: Quaternary International. 279-280, p. 93
Research output: Contribution to journal › Meeting Abstract › Other research output

Cite this

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title = "Response of the Rhine-Meuse fluvial system to Saalian ice-sheet dynamics",

author = "F.S. Busschers and \{van Balen\}, R.T. and K.M. Cohen and C. Kasse and H.J.T. Weerts and J. Wallinga and F.P.M. Bunnik",

year = "2008",

doi = "10.1111/j.1502-3885.2008.00025.x",

language = "English",

volume = "37",

pages = "377--398",

journal = "Boreas",

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TY - JOUR

T1 - Response of the Rhine-Meuse fluvial system to Saalian ice-sheet dynamics

AU - Busschers, F.S.

AU - van Balen, R.T.

AU - Cohen, K.M.

AU - Kasse, C.

AU - Weerts, H.J.T.

AU - Wallinga, J.

AU - Bunnik, F.P.M.

PY - 2008

Y1 - 2008

U2 - 10.1111/j.1502-3885.2008.00025.x

DO - 10.1111/j.1502-3885.2008.00025.x

M3 - Article

SN - 0300-9483

VL - 37

SP - 377

EP - 398

JO - Boreas

JF - Boreas

ER -

Response of the Rhine-Meuse fluvial system to Saalian ice-sheet dynamics

Access to Document

Research output

The successive roles of proglacial drainage, normal ice-age rivers and marine processes in eroding the Strait of Dover and adjacent southernmost North Sea in the last 500 ka

Cite this