Style of deformation and tectono-sedimentary evolution of fold-and-thrust belts and foreland basins: From nature to models - INSU - Institut national des sciences de l'Univers Access content directly
Journal Articles Tectonophysics Year : 2019

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

Stefano Mazzoli
  • Function : Author
Christoph von Hagke
  • Function : Author
Matthias Rosenau
  • Function : Author
Charlotte Fillon
Pablo Granado
  • Function : Author

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.

Dates and versions

insu-03595769 , version 1 (03-03-2022)

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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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