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Solid Earth An interactive open-access journal of the European Geosciences Union
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Volume 8, issue 2
Solid Earth, 8, 405-419, 2017
https://doi.org/10.5194/se-8-405-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
Solid Earth, 8, 405-419, 2017
https://doi.org/10.5194/se-8-405-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 04 Apr 2017

Research article | 04 Apr 2017

Syn-thrusting, near-surface flexural-slipping and stress deflection along folded sedimentary layers of the Sant Corneli-Bóixols anticline (Pyrenees, Spain)

Stefano Tavani1, Pablo Granado2,3, Pau Arbués2,3, Amerigo Corradetti1, and J. Anton Muñoz2,3 Stefano Tavani et al.
  • 1DiSTAR, Università degli Studi di Napoli “Federico II”, Largo S. Marcellino 10, 80138 Naples, Italy
  • 2Institut de Recerca Geomodels, Universitat de Barcelona, Martí i Franquès s/n, 08028 Barcelona, Spain
  • 3Departament de Dinàmica de la Terra i de l'Oceà, Universitat de Barcelona, Martí i Franquès s/n, 08028 Barcelona, Spain

Abstract. In the Spanish Pyrenees, the Sant Corneli-Bóixols thrust-related anticline displays an outstandingly preserved growth strata sequence. These strata lie on top of a major unconformity exposed at the anticline's forelimb that divides and decouples a lower pre-folding unit from an upper syn-folding one. The former consists of steeply dipping to overturned strata with widespread bedding-parallel slip indicative of folding by flexural slip, whereas the syn-folding strata above define a 200m amplitude fold. In the inner and outer sectors of the forelimb, both pre- and syn-folding strata are near vertical to overturned and the unconformity angle ranges from 10 to 30°. In the central portion of the forelimb, syn-folding layers are gently dipping, whereas the angular unconformity is about 90° and the unconformity surface displays strong S–C shear structures, which provide a top-to-foreland slip sense. This sheared unconformity is offset by steeply dipping faults, which are at low angles to the underlying layers of the pre-folding unit. Strong shearing along the unconformity surface also occurred in the inner sector of the forelimb, with S–C structures providing an opposite, top-to-hinterland slip sense. Cross-cutting relationships and slip senses along the pre-folding bedding surfaces and the unconformity indicate that regardless of its orientation, layering in the pre- and syn-folding sequences of the Sant Corneli-Bóixols anticline were continuously slipped. This slipping promoted an intense stress deflection, with the maximum component of the stress tensor remaining at low angles to bedding during most of the folding process.

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In the the Sant Corneli-Bóixols anticline, a syn-growth unconformity divides and de-couples a lower overturned pre-growth unit from an upper syn-growth one. Pre-growth strata and the unconformity underwent syn-folding shearing, even where they are mutually perpendicular. Different and coeval shear senses occurring at different structural positions indicate that regardless of its orientation, layering in the pre- and syn-growth sequences of the anticline was continuously sheared.
In the the Sant Corneli-Bóixols anticline, a syn-growth unconformity divides and de-couples a...
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