3 edition of Fluvial sedimentary geology and chronology of the Holocene Rhine-Meuse delta, the Netherlands found in the catalog.
Fluvial sedimentary geology and chronology of the Holocene Rhine-Meuse delta, the Netherlands
TorbjoМ€rn E. ToМ€rnqvist
|Statement||Torbjörn E. Törnqvist.|
|Series||Nederlandse geografische studies ;, 166|
|LC Classifications||GB1399.9.N4 T67 1993|
|The Physical Object|
|Pagination||169 p. :|
|Number of Pages||169|
|ISBN 10||9068091794, 9062661068|
|LC Control Number||94230980|
The avulsion history of the Holocene Rhine-Meuse delta (The Netherlands) was reconstructed, on a timescale of millenia, using detailed paleogeographic maps based on approximately , Joan Lloret, Ausonio Ronchi, José López-Gómez, Nicola Gretter, Raúl De la Horra, José F. Barrenechea, Alfredo Arche, Syn-tectonic sedimentary evolution of the continental late Palaeozoic-early Mesozoic Erill Castell-Estac Basin and its significance in the development of the central Pyrenees Basin, Sedimentary Geology, /
Fluvial channel and overbank deposits from the Westphalian of the Durham coalfield, NE England. Authors. C. R. FIELDING. Department of Geological Sciences, University of Durham, Science Laboratories, South Road, Durham DH1 3LE, U.K. First published: February Full publication history;. SSDI (94) VITA-FINZI (London, U.K.) Fluvial Sedimentary Geology and Geochronology of the Holocene Rhine-Meuse delta, The Netherlands. T.E. Tornquist. Netherlands Geographical Studies, Utrecht University, , pp., Dfl ISBN
Holocene alternation of meandering and anastomosing fluvial systems in the Rhine-Meuse delta (central Netherlands) controlled by sea-level rise and subsoil erodibility TE Tornqvist Journal of Sedimentary Research 63 (4), , The Holocene Rhine-Meuse delta in the Netherlands offers a unique opportunity to study delta development and resulting deltaic successions at millennial and sub-millennial time resolution over the.
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Read "FLUVIAL SEDIMENTARY GEOLOGY AND CHRONOLOGY OF THE HOLOCENE RHINE–MEUSE DELTA, THE NETHERLANDS by T. Törnqvist, Nederlandse Geografische StudiesUtrecht, No. of pages: Price: Dfl ISBN 90‐‐‐4., Earth Surface Processes and Landforms" on DeepDyve, the largest online rental service for scholarly research with thousands.
Fluvial sedimentary geology and chronology of the Holocene Rhine-Meuse delta, the Netherlands. Utrecht: Koninklijk Nederlands Aardrijkskundig Genootschap, (OCoLC) Material Type: Thesis/dissertation: Document Type: Book: All Authors / Contributors: Torbjörn E Törnqvist. Fluvial sedimentary geology and chronology of the Holocene Rhine–Meuse Delta.
PhD Thesis, Utrecht University. Netherlands Geographical Studies,pp. 1–Cited by: The Schoonrewoerd fluvial system in the central Rhine–Meuse delta was active as a Rhine distributary between and 14 C years BP. Based on planform patterns, cross-sectional facies architecture, reconstructed paleodischarge, and its short period of activity, the Schoonrewoerd fluvial system is interpreted to represent a failed by: Fluvial sedimentary geology and chronology of the Holocene Rhine-Meuse delta, The Netherlands.
Ph.D. Thesis. Nederlandse Geografische Studies Royal Dutch Geographical Society. Faculty of Geographical Sciences, Utrecht University (Utrecht): by: The alluvial architecture of the Holocene Rhine–Meuse delta has been quantified by Gouw () conform the method of Mackey and Bridge () based on five detailed N–S oriented cross sections through the fluvial part of the delta by the following parameters: sand–body width/thickness ratio (SBW/ SBT), channel-belt deposit proportion (CDP.
of the Holocene fluvial sediments to obtain the total volume of. phases in the Holocene sedimentary history of the delta. palaeogeography of the Rhine – Meuse delta, The Netherlands.
Fluvial sedimentary geology and chronology of the Holocene Rhine-Meuse delta, the Netherlands. Ph.D. Thesis Utrecht University, KNAG/Faculteit Ruimtelijke Wetenschappen Universiteit Utrecht, Netherlands Geographical Studiesp. Mid-Holocene water-level changes in the lower Rhine-Meuse delta (western Netherlands): implications for the reconstruction of relative mean sea-level rise, palaeoriver-gradients and coastal evolution.
Netherlands Journal of Geosciences, Vol. 89, Issue. 01, p. Middle Holocene Avulsion-Belt Deposits in the Central Rhine–Meuse Delta, The Netherlands Journal of Sedimentary Research Connecting the backwater hydraulics of coastal rivers to fluvio-deltaic sedimentology and stratigraphy.
Törnqvist, T.E.,Fluvial sedimentary geology and chronology of the Holocene Rhine-Meuse delta, the Netherlands. Utrecht University (Utrecht): pp.
Törnqvist, T.E. & Van Dijk, G.J.,Optimizing sampling strategy for radiocarbon dating of Holocene fluvial systems in a vertically aggrading setting.
The occurrence of alternating meandering and anastomosing fluvial systems in the Holocene Rhine-Meuse Delta (central Netherlands) is discussed here. It is shown that the two fluvial styles not only have distinctive plan morphology but also can be identified on the basis of facies-architectural criteria (width/thickness ratio of channel-belt.
Holocene sea‐level rise resulted in the formation of a coastal prism (Holocene Rhine–Meuse delta). Across the Peel Boundary Fault‐zone (PBF) in the central delta, differences in subsidence between the downstream Roer Valley Graben and its upstream shoulder influenced fluvial deposition.
channels and the upstream parts of the delta. The avulsion history as published in is subtly revised Holocene Rhine-Meuse delta, the Netherlands. The J. of Geol.,insight from the Rhine-Meuse delta. Society for Sedimentary Geology. In: Davidson, S.K. the Holocene Rhine-Meuse delta. A new detailed digital e levation map of the Netherlands, based on very accurate laser-altimetry data, will enable us to map larger areas in greater detail, with greater accuracy, and in a much shorter period of time.
Keywords: geological maps, Holocene, Rhine-Meuse delta, fluvial systems, avulsions. In the lower delta ongoing land subsidence kept creating accommodation space, even during the Late Holocene, when eustatic sea-level rise had tailed out.
Especially between and yr BP FIGURE 2.—The Holocene Rhine–Meuse delta in the central part of the Netherlands. Within the Rhine–Meuse delta, rivers run E–W. Book review Full text access Complex confining layers.
Architecture and hydraulic properties of holocene and late weichselian deposits in the Fluvial Rhine-Meuse delta, The Netherlands: Henk J.T. Weerts. Netherlands Geographical StudiesKNAG/Faculteit Ruimtelijke Wetenschappen Utrecht,paperback, pp., Dfl.
ISBN Quaternary sedimentary and fluvial history in the Upper Rhine of the Holocene Rhine-Meuse delta (The Netherlands): A result of changing external controls five cross-valley sections in the. The alluvial architecture of the Holocene Rhine–Meuse delta (central Netherlands) is strikingly similar to that of the LMV, despite scale differences between the Mississippi and Rhine–Meuse river systems.
Gouw (in press) demonstrated that CDP is ~ in the upstream Rhine–Meuse delta and decreases in a downstream direction to ~ In. Climate and base-level controlled fluvial system change and incision during the last glacial–interglacial transition, Roer river, the Netherlands – western Germany - Volume 96 Issue 2 - C.
Kasse, R.T. Van Balen, S.J.P. Bohncke, J. Wallinga, M. Vreugdenhil. Starting from an overview of the depositional history and (quantified) boundary conditions of the Holocene Rhine–Meuse delta, The Netherlands, this paper discusses the implications of avulsions for fluvial-deltaic architecture based on extensive field data, highlighting the geometric properties, channel-deposit proportion (CDP), channelbelt.Ingwer J.
Bos, Esther Stouthamer, Spatial and Temporal Distribution of Sand-Containing Basin Fills in the Holocene Rhine-Meuse Delta, the Netherlands, The Journal of Geology, /,6, (), ().Book review Full text access Fluvial sedimentary geology and geochronology of the Holocene Rhine-Meuse delta, The Netherlands: T.E.
Tornquist. Netherlands Geographical Studies, Utrecht University,pp., Dfl ISBN