This article is an erratum on:
Quantifying the mechanisms of rain-triggered seismicity in karstic regions
Frontiers Production OfficeAn Erratum on
Quantifying the mechanisms of rain-triggered seismicity in karstic regions
by Perrochet L, Preisig G and Valley B (2023). Front. Earth Sci. 11:1234856. doi: 10.3389/feart.2023.1234856
Due to a production error, some text elements were incorrectly copyedited.
The following corrections have been made to the Abstract:
“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 Karst geology, triggering mechanisms, and conceptual model, subsection 2.1 Karst-specific features, first paragraph:
“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 Karst geology, triggering mechanisms, and conceptual model, subsection 2.3 Conceptual model, first paragraph:
“[…] (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.
Keywords: karst, rain-triggered, seismicity, pore-pressure, diffusion
Citation: Frontiers Production Office (2023) Erratum: Quantifying the mechanisms of rain-triggered seismicity in karstic regions. Front. Earth Sci. 11:1347081. doi: 10.3389/feart.2023.1347081
Received: 30 November 2023; Accepted: 30 November 2023;
Published: 11 December 2023.
Approved by:
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