Tectonophysics 611 (2014) 204

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Corrigendum

Corrigendum to “Numerical modelling of magma transport in dykes” [Tectonophysics 526–529 (2012) 97–109] P. Yamato a,b,⁎, R. Tartèse a, T. Duretz b, D.A. May b a b

Géosciences Rennes, CNRS UMR 6118, Université de Rennes 1, 35042 Rennes Cedex, France Institute of Geophysics, Department of Earth Science, ETH-Zurich, Sonneggstrasse 5, CH-8092 Zurich, Switzerland

The results presented in Figure 9 were obtained using an imposed block velocity (Vzblock) and the corresponding pressure gradients (Pdriv) assuming an incorrect dyke thickness (Wd) of 1 m, instead of the correct value of Wd = 0.5 m. According to Equation 9, for a given Vzblock, the value of Pdriv should be 4 times lower in a 1 m dyke than in a 0.5 m dyke. Hence, in order to correctly scale the results (i.e., to obtain the same behaviour in 0.5 m dyke than in a 1 m dyke), the time scales shown in Figure 9 need to be increased by a factor 4 and values of Pdriv reported need to be decreased by a factor 4. As an example, the corrected Figure 9 for Intermediate Vz experiment thus becomes:

The authors apologise for this mistake, which nevertheless, do not affect the general conclusions of this paper.

DOI of original article: http://dx.doi.org/10.1016/j.tecto.2011.05.015. ⁎ Corresponding author: Géosciences Rennes, CNRS UMR 6118, Université de Rennes 1, 35042 Rennes Cedex, France. Tel.: +33 2 23 23 60 95. E-mail address: [email protected] (P. Yamato). 0040-1951/$ – see front matter © 2013 Elsevier B.V. All rights reserved. http://dx.doi.org/10.1016/j.tecto.2013.11.031