Effect of lithosphere thickness heterogeneities in controlling rift localization: Numerical modeling of the Oslo Graben

Physics

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Tectonophysics: Continental Margins And Sedimentary Basins (1212), Tectonophysics: Continental Tectonics-Extensional (0905), Tectonophysics: Dynamics Of Lithosphere And Mantle-General, Tectonophysics: Rheology-Crust And Lithosphere, Structural Geology: Local Crustal Structure

Scientific paper

We present 2-D thermo-mechanical and numerical modeling at lithospheric scale to assess the impact of pre-existing lithosphere thickness contrast on rift localization. The results of the modeling suggest that thickness heterogeneity was responsible for focussing rifting and passive asthenospheric upwelling in the Permo-Carboniferous Oslo Graben at the western margin of the Fennoscandian Shield. These findings are consistent with inferences from recent studies showing that both the crust-mantle boundary and the base of the lithosphere are and were deeper at the eastern margin of the Oslo Graben, resulting in contrasting crust and lithosphere thickness.

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