Zobrazeno 1 - 10
of 57
pro vyhledávání: '"J. D. Jansen"'
Publikováno v:
Earth Surface Dynamics, Vol 12, Pp 953-971 (2024)
River terraces are frequently investigated with the aim of extracting information regarding tectonic or climate forcing on the evolution of landscapes. Terraces formed following the blockage of valleys by large-scale landsliding have received limited
Externí odkaz:
https://doaj.org/article/fe76a920a4a14cd08647324e6b6ecff4
Publikováno v:
Geomechanics and Geophysics for Geo-Energy and Geo-Resources, Vol 9, Iss 1, Pp 1-18 (2023)
Abstract Recent laboratory and field studies suggest that temporal variations in injection patterns (e.g., cyclic injection) might trigger less seismicity than constant monotonic injection. This study presents results from uniaxial compressive experi
Externí odkaz:
https://doaj.org/article/4b97591ddf12427bb507505bc23019ee
Publikováno v:
Earth Surface Dynamics, Vol 11, Pp 865-880 (2023)
By simulating erosion and deposition, landscape evolution models (LEMs) offer powerful insights into Earth surface processes and dynamics. Stream-power-based LEMs are often constructed from parameters describing drainage area (m), slope (n), substrat
Externí odkaz:
https://doaj.org/article/a1e02183bd89436eb4d5cfaf01707395
Publikováno v:
Earth Surface Dynamics, Vol 11, Pp 817-833 (2023)
Rock slope failures in the Lake District, UK, have been associated with deglacial processes after the Last Glacial Maximum, but the controls and timing of the failures remain poorly known. A cirque headwall failure was investigated to determine failu
Externí odkaz:
https://doaj.org/article/0b0f51e29aa24be592f4f922e2087857
Autor:
M. Struck, J. D. Jansen, T. Fujioka, A. T. Codilean, D. Fink, R.-H. Fülöp, K. M. Wilcken, D. M. Price, S. Kotevski, L. K. Fifield, J. Chappell
Publikováno v:
Earth Surface Dynamics, Vol 6, Pp 329-349 (2018)
Sediment-routing systems continuously transfer information and mass from eroding source areas to depositional sinks. Understanding how these systems alter environmental signals is critical when it comes to inferring source-area properties from the
Externí odkaz:
https://doaj.org/article/4bb628e1a46744a9a804bffaeedf5e65
Publikováno v:
Earth Surface Dynamics, Vol 3, Iss 4, Pp 447-462 (2015)
With accelerating climate cooling in the late Cenozoic, glacial and periglacial erosion became more widespread on the surface of the Earth. The resultant shift in erosion patterns significantly changed the large-scale morphology of many mountain r
Externí odkaz:
https://doaj.org/article/84f320210ba841ca9936dd69fbca4fb2
Publikováno v:
Earth Surface Dynamics, Vol 3, Iss 4, Pp 463-482 (2015)
There is growing recognition of strong periglacial control on bedrock erosion in mountain landscapes, including the shaping of low-relief surfaces at high elevations (summit flats). But, as yet, the hypothesis that frost action was crucial to the
Externí odkaz:
https://doaj.org/article/ed446b6644c24e5d9eb622108f157650
Akademický článek
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Akademický článek
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Autor:
W. Schut, J. D. Jansen
Publikováno v:
Recueil des Travaux Chimiques des Pays-Bas. 51:321-341