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Frédéric Mouthereau

Researcher at Paul Sabatier University

Publications -  95
Citations -  5658

Frédéric Mouthereau is an academic researcher from Paul Sabatier University. The author has contributed to research in topics: Foreland basin & Tectonics. The author has an hindex of 39, co-authored 86 publications receiving 4690 citations. Previous affiliations of Frédéric Mouthereau include University of Toulouse & Pierre-and-Marie-Curie University.

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Convergence history across Zagros (Iran): constraints from collisional and earlier deformation

TL;DR: In this paper, the main Zagros orogen is shown to be deeply rooted, possibly to Moho depths, and the suture zone effectively runs along the MZT.
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Building the Zagros collisional orogen: Timing, strain distribution and the dynamics of Arabia/Eurasia plate convergence

TL;DR: In this paper, the authors show that only 42% of the post-35 Ma convergence is partitioned by shortening within central Iran, and the current subduction dynamics can be explained by the original lateral difference in the buoyancy of the distal margin.
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Late Cenozoic and modern stress fields in the western Fars (Iran): Implications for the tectonic and kinematic evolution of central Zagros

TL;DR: In this paper, the inversion of focal mechanisms from small and moderate earthquakes shows a consistent N020°-030° compression with a low ratio between differential stresses. But the authors do not consider the impact of small earthquakes on the stability of the strike-slip faults.
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Tertiary sequence of deformation in a thin‐skinned/thick‐skinned collision belt: The Zagros Folded Belt (Fars, Iran)

TL;DR: In this article, the authors describe how thin-skinned/thick-skinned deformation in the Zagros Folded Belt interacted in time and space, and estimate a total shortening of 65-78 km (16-19%).
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Placing limits to shortening evolution in the Pyrenees: Role of margin architecture and implications for the Iberia/Europe convergence

TL;DR: In this paper, the authors combine existing and new sequentially restored cross sections in the central Pyrenees, with Iberia/Europe (IB/EU) plate kinematic reconstructions and new apatite fission track, zircon (U-Th)/He, and U/Pb ages to discuss higher and lower bounds of crustal shortening and determine the amount of distal margin sutured during collision.