Did the Variscides collapse or were they torn apart?: A quantitative evaluation of the driving forces for postconvergent extension in central Europe
Article Abstract:
Extension after the end of convergence led to rapid destruction of the European Variscan orogen and caused the formation of sedimentary basins and widespread magmatism. The possible driving forces such as gravitational collapse or reorientation of the far-field stress regime, are examined using a two-dimensional thermo-mechanical finite element modeling approach.
Publication Name: Tectonics
Subject: Earth sciences
ISSN: 0278-7407
Year: 1999
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Palinspastic restoration of a post-Taconian successor basin deformed within a transpressive regime, northern Appalachians
Article Abstract:
Restoration of the post-Taconian successor basin, the Gaspe Belt, situated in the external area of the Acadian orogen in the Canadian Appalachians, was undertaken with a step-by-step process based on the successive removal of strain increments. This was undertaken taking into consideration the pure shear and simple shear parts of the transpressive deformation.
Publication Name: Tectonics
Subject: Earth sciences
ISSN: 0278-7407
Year: 1999
User Contributions:
Comment about this article or add new information about this topic:
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