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Style of deformation and tectono-sedimentary evolution of fold-and-thrust belts and foreland basins: From nature to models

Abstract : Orogenic systems, including their external fold-and-thrust belts and foreland basin systems, generally evolve from the inversion and imbrication of former continental margins. Continental margins are characterized by displaying along-strike variations in the degree of inherited regional extension (i.e., from limited lithospheric stretching to full necking, leading to mantle exhumation and oceanic accretion). These differences have a fundamental impact on the pre-shortening thermal state of the lithosphere and on structural style development.
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https://hal-insu.archives-ouvertes.fr/insu-03595769
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Submitted on : Thursday, March 3, 2022 - 12:58:56 PM
Last modification on : Saturday, March 5, 2022 - 3:31:03 AM

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Olivier Lacombe, Stefano Mazzoli, Christoph von Hagke, Matthias Rosenau, Charlotte Fillon, et al.. Style of deformation and tectono-sedimentary evolution of fold-and-thrust belts and foreland basins: From nature to models. Tectonophysics, 2019, 767, pp. 4567-4587. ⟨10.1016/j.tecto.2019.228163⟩. ⟨insu-03595769⟩

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