@misc{ mendeley_4733892521,
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  abstract = {The geology of Western and Central Europe is significantly influenced by the Variscan orogen that developed during Devonian and Carboniferous time. Numerical models are essential in understanding and quantifying the involved endogenous and exogenous processes and their interactions. These are mainly based on the large-scale mass redistribution caused by erosion and fluvial sed- imentary transport. The sedimentary mass flux leads to changing loads on the lithosphere and affects therefore the evolution of the orogen and the foreland-basin. The complex feedback-mechanism of the surface and tectonic processes is studied by three-dimensional elastic–plastic numerical models. The calculated uplift rates are used to model the interaction between tectonic and surface processes such as erosion and sedimentation. An iterative application of the numerical models for the tectonic and surface processes yields a detailed view of the evolution of the foreland-basin. The tectonic model itself (excluding surface processes) already shows some of the palinspastically reconstructed important features of the lower Carboniferous like the London-Brabant Massif, and the northward propagation of the Variscan deformation front. The results obtained from the coupled analysis can be compared to studies of the sedimentary record (i.e. time, thickness, and sedimentation rates) and other geological concepts (i.e. stability of geological provinces). The results demonstrate that both processes are essential in understanding the complex structural evolution of the Variscides and their foreland. The numerical approach on the tectonic–surface process interaction can also be applied easily to other geological settings.},
  month = {1},
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  year = {2004},
  keywords = {Constraints, Elastic-Plastic Rheology, Elastic–plastic rheology, Numerical modelling, Surface processes, Tectonic processes},
  isstarred = {1},
  id = {4733892521},
  discipline = {Earth Sciences},
  address = {Ruhr Univ Bochum, Inst Geol Mineral & Geophys, D-44780 Bochum, Germany},
  title = {Evolution of the Variscan foreland-basin: modelling the interactions between tectonics and surface processes},
  day = {1},
  deletionpending = {0},
  version = {1372700178},
  issue = {10},
  url_pdf_0 = {http://www.mendeley.com/download/public/5129541/4733892521/795ff4b825329f4571d70b8474d44fc9953fcf82/dl.pdf},
  url_mendeley = {http://www.mendeley.com//research/evolution-variscan-foreland-basin-modelling-interactions-between-tectonics-surface-processes//},
  source_type = {JOUR},
  isread = {1},
  author = {Kasper David {Fischer} and Thomas {Jahr} and Gerhard {Jentzsch}},
  series = {Physics and Chemistry of the Earth, Parts A/B/C},
  pages = {665-671},
  volume = {29},
  doi = {10.1016/j.pce.2004.03.004},
  url = {http://www.sciencedirect.com/science?_ob=ArticleURL&_udi=B6X1W-4C60353-2&_user=2873218&_rdoc=1&_fmt=&_orig=search&_sort=d&_docanchor=&view=c&_acct=C000059020&_version=1&_urlVersion=0&_userid=2873218&md5=75a238661e48a183cbb8db9de83afa83
papers://b0c4ae4e-957c-4898-a5c3-421bbafd443e/Paper/p88
http://linkinghub.elsevier.com/retrieve/pii/S1474706504000695},
  type = {Journal Article},
  issn = {14747065},
  modified = {1372700178},
  subdiscipline = {Seismology/Seismics},
  booktitle = {Physics and Chemistry of the Earth, Parts A/B/C},
  dateaccessed = {29/05/11}
}

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The tectonic model itself (excluding surface processes) already shows some of the palinspastically reconstructed important features of the lower Carboniferous like the London-Brabant Massif, and the northward propagation of the Variscan deformation front. The results obtained from the coupled analysis can be compared to studies of the sedimentary record (i.e. time, thickness, and sedimentation rates) and other geological concepts (i.e. stability of geological provinces). The results demonstrate that both processes are essential in understanding the complex structural evolution of the Variscides and their foreland. 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