Zobrazeno 1 - 10
of 15
pro vyhledávání: '"R.F. Houtgast"'
Publikováno v:
Quaternary Science Reviews. 24:439-454
Earthquakes and vertical land movements inferred from geodetic levelling results demonstrate that the Netherlands is situated on a tectonically active part of the Earth's surface. Tectonic subsidence analyses of the sedimentary records in the basins
Publikováno v:
van Balen, R T, Houtgast, R F, van der Wateren, F M & Vandenberghe, J 2002, ' Neotectonic evolution and sediment budget of the Meuse catchment in the Ardennes and the Roer Valley Rift System ', Netherlands Journal of Geosciences = Geologie en Mijnbouw, vol. 81, pp. 211-215 . https://doi.org/10.1017/S0016774600022459
Netherlands Journal of Geosciences = Geologie en Mijnbouw, 81, 211-215. Koninklijk Nederlands Geologisch Mijnbouwkundig Genootschap
Netherlands Journal of Geosciences = Geologie en Mijnbouw, 81, 211-215. Koninklijk Nederlands Geologisch Mijnbouwkundig Genootschap
Using marine planation surfaces, fluvial terraces and a digital terrain model, the amount of eroded rock volume versus time for the Meuse catchment has been computed. A comparison of the amount of eroded volume with the volume of sediment preserved i
Publikováno v:
Tectonophysics. 352:295-315
The Meuse River crosses the Feldbiss Fault Zone, one of the main border fault zones of the Roer Valley Graben in the southern part of the Netherlands. Uplift of the area south of the Feldbiss Fault Zone forced the Meuse River to incise and, as a resu
Autor:
R.T. van Balen, R.F. Houtgast
Publikováno v:
Global and Planetary Change, 27, 107-123. Elsevier
Houtgast, R F & van Balen, R T 2000, ' Neotectonics of the Roer Valley Rift System, the Netherlands. ', Global and Planetary Change, vol. 27, pp. 107-123 . https://doi.org/10.1016/S0921-8181(01)00063-7
Houtgast, R F & van Balen, R T 2000, ' Neotectonics of the Roer Valley Rift System, the Netherlands. ', Global and Planetary Change, vol. 27, pp. 107-123 . https://doi.org/10.1016/S0921-8181(01)00063-7
The Roer Valley Rift System (RVRS) is located in the southern part of the Netherlands and adjacent parts of Germany and Belgium. The last rifting episode of the RVRS started in the Late Oligocene and is still ongoing. The present-day seismic activity
Publikováno v:
Houtgast, R F, van Balen, R T & Kasse, C 2005, ' Late Quaternary tectonic evolution of the Feldbiss Fault (Roer Valley Rift System, The Netherlands) based on trenching, and its potential relation to glacial unloading ', Quaternary Science Reviews, vol. 24, pp. 491-510 . https://doi.org/10.1016/j.quascirev.2004.01.012
Quaternary Science Reviews, 24, 491-510. Elsevier Limited
Quaternary Science Reviews, 24, 491-510. Elsevier Limited
The most important tectonic structure in the southern part of the Netherlands is the Roer Valley Rift System (RVRS). The main border fault zones of the RVRS, the Peel Boundary and the Feldbiss Fault zones, have been active during the Quaternary and a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::57f44a962849ddcc9022b3c96a91f7c9
https://hdl.handle.net/1871.1/1400b477-1647-491c-9c4b-3a9392128289
https://hdl.handle.net/1871.1/1400b477-1647-491c-9c4b-3a9392128289
Publikováno v:
Netherlands Journal of Geosciences = Geologie en Mijnbouw, 82-2, 177-196. Koninklijk Nederlands Geologisch Mijnbouwkundig Genootschap
Houtgast, R F, van Balen, R T, Kasse, C & Vandenberghe, J 2003, ' Late Quaternary tectonic evolution and postseismic near surface fault displacements along the Geleen Fault (Feldbiss Fault Zone-Roer Valley Rift System, the Netherlands) based on trenching. ', Netherlands Journal of Geosciences = Geologie en Mijnbouw, vol. 82-2, pp. 177-196 . https://doi.org/10.1017/S0016774600020734
Houtgast, R F, van Balen, R T, Kasse, C & Vandenberghe, J 2003, ' Late Quaternary tectonic evolution and postseismic near surface fault displacements along the Geleen Fault (Feldbiss Fault Zone-Roer Valley Rift System, the Netherlands) based on trenching. ', Netherlands Journal of Geosciences = Geologie en Mijnbouw, vol. 82-2, pp. 177-196 . https://doi.org/10.1017/S0016774600020734
In northwest Europe the pattern of earthquake distribution is correlated with known Quaternary faults. Excavation of fault scarps revealed that these fault zones have been active during the Late Pleistocene. In this paper we present the results of an
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::54b652d3bc57b2e6828206585c40e121
https://research.vu.nl/en/publications/1417c8bd-d975-4904-b596-471052de09ad
https://research.vu.nl/en/publications/1417c8bd-d975-4904-b596-471052de09ad
Publikováno v:
EAGE Conference on Exploring the Synergies between Surface and Borehole Geoscience - Petrophysics meets Geophysics.
Publikováno v:
Global and Planetary Change, 271, 89-106. Elsevier
van Balen, R T, Houtgast, R F, van der Wateren, F M, Vandenberghe, J & Bogaart, P W 2000, ' Sediment budget and tectonic evolution of the Meuse catchment in the Ardennes and the Roer Valley Rift System. ', Global and Planetary Change, vol. 271, pp. 89-106 . https://doi.org/10.1016/S0921-8181(01)00062-5
Global and Planetary Change, 1-4, 27, 113-129
van Balen, R T, Houtgast, R F, van der Wateren, F M, Vandenberghe, J & Bogaart, P W 2000, ' Sediment budget and tectonic evolution of the Meuse catchment in the Ardennes and the Roer Valley Rift System. ', Global and Planetary Change, vol. 271, pp. 89-106 . https://doi.org/10.1016/S0921-8181(01)00062-5
Global and Planetary Change, 1-4, 27, 113-129
The Meuse river system is located in the northeastern part of the Paris Basin, the Ardennes, and the Roer Valley Rift System (RVRS). The Meuse river system developed during the uplift of the Ardennes since the Eocene and it was affected by renewed ri
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::00dec6efaaecef5dd8edd749e95bfc5a
http://resolver.tudelft.nl/uuid:a2965e58-b941-4f30-97a0-dfb44b420ee9
http://resolver.tudelft.nl/uuid:a2965e58-b941-4f30-97a0-dfb44b420ee9
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Akademický článek
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