Plan
Comptes Rendus
no. 9

Corrigendum to the note “Evidence of Quaternary active folding near Utique (Northeast Tunisia) from tectonic observations and a seismic profile” [C. R. Geoscience 342 (11) (2010) 864–72]
[Corrigendum à la note « Evidence of Quaternary active folding near Utique (Northeast Tunisia) from tectonic observations and a seismic profile » [C. R. Geoscience 342 (11) (2010) 864–72]]
Lassaad Mejri1, 2, 3, 4, 5 ; Vincent Regard1, 2, 3  ; Sébastien Carretier1, 2, 3 ; Stéphane Brusset1, 2, 3 ; Mahmoud Dlala5
1 Université de Toulouse, UPS (OMP), LMTG, 14, avenue Édouard-Belin, 31400 Toulouse, France
2 CNRS, LMTG, 31400 Toulouse, France
3 IRD, LMTG, 31400 Toulouse, France
4 CNSTN, pôle technologique, 2020 Sidi Thabet, Ariana, Tunisia
5 Faculté des sciences de Tunis, université de Tunis El Manar, 1060 Tunis, Tunisia
Comptes Rendus. Géoscience, Volume 344 (2012) no. 9, p. 471.
fait référence à Evidence of Quaternary active folding near Utique (Northeast Tunisia) from tectonic observations and a seismic profile
[Plissement quaternaire d’Utique (nord-est de la Tunisie) : mise en évidence par des observations tectoniques et une ligne sismique]
Métadonnées
Publié le :
DOI : 10.1016/j.crte.2012.08.007

Lassaad Mejri 1, 2, 3, 4, 5 ; Vincent Regard 1, 2, 3 ; Sébastien Carretier 1, 2, 3 ; Stéphane Brusset 1, 2, 3 ; Mahmoud Dlala 5

1 Université de Toulouse, UPS (OMP), LMTG, 14, avenue Édouard-Belin, 31400 Toulouse, France
2 CNRS, LMTG, 31400 Toulouse, France
3 IRD, LMTG, 31400 Toulouse, France
4 CNSTN, pôle technologique, 2020 Sidi Thabet, Ariana, Tunisia
5 Faculté des sciences de Tunis, université de Tunis El Manar, 1060 Tunis, Tunisia 
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     author = {Lassaad Mejri and Vincent Regard and S\'ebastien Carretier and St\'ephane Brusset and Mahmoud Dlala},
     title = {Corrigendum to the note {{\textquotedblleft}Evidence} of {Quaternary} active folding near {Utique} {(Northeast} {Tunisia)} from tectonic observations and a seismic profile{\textquotedblright} {[C.} {R.} {Geoscience} 342 (11) (2010) 864{\textendash}72]},
     journal = {Comptes Rendus. G\'eoscience},
     pages = {471},
     publisher = {Elsevier},
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Lassaad Mejri; Vincent Regard; Sébastien Carretier; Stéphane Brusset; Mahmoud Dlala. Corrigendum to the note “Evidence of Quaternary active folding near Utique (Northeast Tunisia) from tectonic observations and a seismic profile” [C. R. Geoscience 342 (11) (2010) 864–72]. Comptes Rendus. Géoscience, Volume 344 (2012) no. 9, p. 471. doi : 10.1016/j.crte.2012.08.007. https://comptes-rendus.academie-sciences.fr/geoscience/articles/10.1016/j.crte.2012.08.007/

Version originale du texte intégral

There is a scale problem between the text and Figure 5. Figure 5 is correct.

Hence in the text (Abstract and sections 4.1 Seismic profiles, and 5. Discussion):

  • • the total shortening is 275 m and not 690 m;
  • • the Plio-Pleistocene shortening rate is 0.55 mm/yr instead of 0.14 mm/yr;
  • • with the assumption shortening occurred only during Pleistocene, the shortening rate is 0.15 mm/yr instead of 0.38 mm/yr (that is, 3% and not 8% of the current shortening in Tunisia).

The other conclusions remain unchanged.

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