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Retro-wedge foreland basin evolution along the ECORS line, eastern Pyrenees, France

Abstract : The eastern Aquitaine basin and North Pyrenean Zone show many characteristics of retro-wedge models. However, they differ significantly in that slow subsidence and low deformation continued throughout orogenesis so that growth and steady-state phases cannot be distinguished. We show that the eastern Pyrenees record two clear phases of convergence and probably never attained steady state. Analysis of the Aquitaine retro-foreland basin along the Ariège ECORS deep seismic line, eastern French Pyrenees, integrates a new litho- and chronostratigraphy, subsidence analysis, low-temperature thermochronology data, new interpretations of seismic lines and a balanced cross-section. Within an overall regression, two shallowing-up cycles (Latest Santonian–Danian, Thanetian–Oligocene) record slow tectonic subsidence of the eastern Aquitaine basin separated by a quiet period. Continuing thick-skinned shortening was low to moderate. The early marine basin, generated by loading of the weak, extended margin, was supplied axially from an unknown eastern edifice while the young Pyrenean orogeny to the south remained submerged. During the quiet period of ultra-slow subsidence, no basin migration and negligible sediment supply, continental conditions characterized the eastern orogen. The second marine transgression was quickly followed by continental conditions. The basin was supplied by the now emerging Pyrenean orogen and continued to subside until Miocene time.
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https://hal-insu.archives-ouvertes.fr/insu-01392395
Contributor : Isabelle Dubigeon <>
Submitted on : Friday, November 4, 2016 - 12:45:28 PM
Last modification on : Monday, June 22, 2020 - 7:54:04 AM

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Mary Ford, Louis Hemmer, Arnaud Vacherat, Kerry Gallagher, Frédéric Christophoul. Retro-wedge foreland basin evolution along the ECORS line, eastern Pyrenees, France. Journal of the Geological Society, Geological Society, 2016, 173 (5), pp.419-437. ⟨10.1144/jgs2015-129⟩. ⟨insu-01392395⟩

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