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Due to a production error, some text elements were incorrectly copyedited.
The following corrections have been made to the
“This generates rapid and large variations in hydraulic head, possibly leading to large changes in pore pressure at seismogenic depth.”
“Results show that the pore pressure increase resulting from the crustal loading and poroelastic deformation is much smaller than the pore pressure increase resulting from a direct hydraulic connection and its diffusion towards depth over small distances.”
A correction has been made to Section 2
“Mature karst systems consist in well developed channels of various morphologies within a relatively low permeable rock matrix, typically consisting of soluble rocks such as limestones, dolomites or evaporites.”
A correction has been made to Section 2
“[…] (iii) a delayed response due to fluid migration towards depth.”
The publisher apologizes for this mistake. The original version of this article has been updated.