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- W2091597527 abstract "Progressive unconformities result from a simultaneous interference of sedimentation, erosion, and tectonic processes. For the purpose of simulating the geometry of these structures occurring on the front of active folds in foreland basin margins, we propose a 2D forward kinematic model. By analogy to several natural examples of syntectonic basins, the syncline frontal hinge typically displays a curved rather than a kinked shape. This model is incremental, and assumes that deformation in the limb of growth strata consists of simple shear parallel to pregrowth strata. It is possible to introduce erosional events at any time of kinematics history. Syntectonic basins associated to emergent structures were modelled, focusing on the syncline frontal hinge and the forelimb of the anticline, without regarding the type of fold. We show that growth stratal final geometry is closely dependent on (1) the behaviour of the synclinal hinge (hinge migration model versus limb rotation model); (2) the erosion of pre- and syntectonic beds, and the attitude of the erosional surface; (3) the evolution of the (R) ratio (amount of deformation/sediment thickness). Simulating several theoretical tectono-sedimentary scenarios, we show how growth strata geometry provides a very fine recording of every variation of the (R) ratio during amplification of folding. As an example, we propose a kinematic evolution for the classical Sant Llorenc de Morunys structures, resulting from its forward reconstruction." @default.
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- W2091597527 date "2002-01-01" @default.
- W2091597527 modified "2023-10-05" @default.
- W2091597527 title "Forward modelling of foreland basins progressive unconformities" @default.
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- W2091597527 doi "https://doi.org/10.1016/s0037-0738(01)00167-1" @default.
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