Sedimentary architecture and optical dating of Middle and Late Pleistocene Rhine-Meuse deposits – fluvial response to climate change, sea-level fluctuation and glaciation
Eight continuous corings in the west-central Netherlands show a 15 to 25 m thick stacked sequence of sandy to gravelly channel-belt deposits of the Rhine-Meuse system. This succession of fluvial sediments was deposited under net subsiding conditions in the southern part of the North Sea Basin and do...
Main Authors: | , , , , , , |
---|---|
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Netherlands Journal of Geosciences’ Foundation
2005
|
Subjects: | |
Online Access: | http://resolver.tudelft.nl/uuid:95d68c7d-4b4f-46b2-928d-72e4801a9641 |
id |
fttudelft:oai:tudelft.nl:uuid:95d68c7d-4b4f-46b2-928d-72e4801a9641 |
---|---|
record_format |
openpolar |
spelling |
fttudelft:oai:tudelft.nl:uuid:95d68c7d-4b4f-46b2-928d-72e4801a9641 2023-07-30T04:06:18+02:00 Sedimentary architecture and optical dating of Middle and Late Pleistocene Rhine-Meuse deposits – fluvial response to climate change, sea-level fluctuation and glaciation Busschers, F.S. (author) Weerts, H.J.T. (author) Wallinga, J. (author) Cleveringa, P. (author) Kasse, C. (author) De Wolf, H. (author) Cohen, K.M. (author) 2005-03-01 http://resolver.tudelft.nl/uuid:95d68c7d-4b4f-46b2-928d-72e4801a9641 en eng Netherlands Journal of Geosciences’ Foundation Netherlands Journal of Geosciences, Geologie en Mijnbouw 84, 1, 25- 41, 2005--00167746 http://resolver.tudelft.nl/uuid:95d68c7d-4b4f-46b2-928d-72e4801a9641 (c) Stichting Netherlands Journal of Geosciences journal article Text 2005 fttudelft 2023-07-08T20:14:43Z Eight continuous corings in the west-central Netherlands show a 15 to 25 m thick stacked sequence of sandy to gravelly channel-belt deposits of the Rhine-Meuse system. This succession of fluvial sediments was deposited under net subsiding conditions in the southern part of the North Sea Basin and documents the response of the Rhine-Meuse river system to climate and sea-level change and to the glaciation history. On the basis of grain size characteristics, sedimentological structures, nature and extent of bounding surfaces and palaeo-ecological data, the sequence was subdivided into five fluvial units, an estuarine and an aeolian unit. Optical dating of 34 quartz samples showed that the units have intra Saalian to Weichselian ages (Marine Isotope Stages 8 to 2). Coarse-grained fluvial sediments primarily deposited under cold climatic conditions, with low vegetation cover and continuous permafrost. Finer-grained sediments generally deposited during more temperate climatic conditions with continuous vegetation cover and/or periods of sea-level highstand. Most of the sedimentary units are bounded by unconformities that represent erosion during periods of climate instability, sea-level fall and/or glacio-isostatic uplift Applied Sciences Article in Journal/Newspaper permafrost Delft University of Technology: Institutional Repository |
institution |
Open Polar |
collection |
Delft University of Technology: Institutional Repository |
op_collection_id |
fttudelft |
language |
English |
description |
Eight continuous corings in the west-central Netherlands show a 15 to 25 m thick stacked sequence of sandy to gravelly channel-belt deposits of the Rhine-Meuse system. This succession of fluvial sediments was deposited under net subsiding conditions in the southern part of the North Sea Basin and documents the response of the Rhine-Meuse river system to climate and sea-level change and to the glaciation history. On the basis of grain size characteristics, sedimentological structures, nature and extent of bounding surfaces and palaeo-ecological data, the sequence was subdivided into five fluvial units, an estuarine and an aeolian unit. Optical dating of 34 quartz samples showed that the units have intra Saalian to Weichselian ages (Marine Isotope Stages 8 to 2). Coarse-grained fluvial sediments primarily deposited under cold climatic conditions, with low vegetation cover and continuous permafrost. Finer-grained sediments generally deposited during more temperate climatic conditions with continuous vegetation cover and/or periods of sea-level highstand. Most of the sedimentary units are bounded by unconformities that represent erosion during periods of climate instability, sea-level fall and/or glacio-isostatic uplift Applied Sciences |
format |
Article in Journal/Newspaper |
author |
Busschers, F.S. (author) Weerts, H.J.T. (author) Wallinga, J. (author) Cleveringa, P. (author) Kasse, C. (author) De Wolf, H. (author) Cohen, K.M. (author) |
spellingShingle |
Busschers, F.S. (author) Weerts, H.J.T. (author) Wallinga, J. (author) Cleveringa, P. (author) Kasse, C. (author) De Wolf, H. (author) Cohen, K.M. (author) Sedimentary architecture and optical dating of Middle and Late Pleistocene Rhine-Meuse deposits – fluvial response to climate change, sea-level fluctuation and glaciation |
author_facet |
Busschers, F.S. (author) Weerts, H.J.T. (author) Wallinga, J. (author) Cleveringa, P. (author) Kasse, C. (author) De Wolf, H. (author) Cohen, K.M. (author) |
author_sort |
Busschers, F.S. (author) |
title |
Sedimentary architecture and optical dating of Middle and Late Pleistocene Rhine-Meuse deposits – fluvial response to climate change, sea-level fluctuation and glaciation |
title_short |
Sedimentary architecture and optical dating of Middle and Late Pleistocene Rhine-Meuse deposits – fluvial response to climate change, sea-level fluctuation and glaciation |
title_full |
Sedimentary architecture and optical dating of Middle and Late Pleistocene Rhine-Meuse deposits – fluvial response to climate change, sea-level fluctuation and glaciation |
title_fullStr |
Sedimentary architecture and optical dating of Middle and Late Pleistocene Rhine-Meuse deposits – fluvial response to climate change, sea-level fluctuation and glaciation |
title_full_unstemmed |
Sedimentary architecture and optical dating of Middle and Late Pleistocene Rhine-Meuse deposits – fluvial response to climate change, sea-level fluctuation and glaciation |
title_sort |
sedimentary architecture and optical dating of middle and late pleistocene rhine-meuse deposits – fluvial response to climate change, sea-level fluctuation and glaciation |
publisher |
Netherlands Journal of Geosciences’ Foundation |
publishDate |
2005 |
url |
http://resolver.tudelft.nl/uuid:95d68c7d-4b4f-46b2-928d-72e4801a9641 |
genre |
permafrost |
genre_facet |
permafrost |
op_relation |
Netherlands Journal of Geosciences, Geologie en Mijnbouw 84, 1, 25- 41, 2005--00167746 http://resolver.tudelft.nl/uuid:95d68c7d-4b4f-46b2-928d-72e4801a9641 |
op_rights |
(c) Stichting Netherlands Journal of Geosciences |
_version_ |
1772818831762259968 |