Articles | Volume 11, issue 6
Solid Earth, 11, 2549–2556, 2020
https://doi.org/10.5194/se-11-2549-2020
Solid Earth, 11, 2549–2556, 2020
https://doi.org/10.5194/se-11-2549-2020

Peer-reviewed comment 23 Dec 2020

Peer-reviewed comment | 23 Dec 2020

Comment on “Estimating the depth and evolution of intrusions at resurgent calderas: Los Humeros (Mexico)” by Urbani et al. (2020)

Gianluca Norini and Gianluca Groppelli

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Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Gianluca Norini on behalf of the Authors (17 Nov 2020)  Author's response    Manuscript
ED: Publish as is (20 Nov 2020) by Joachim Gottsmann
ED: Publish as is (20 Nov 2020) by Joachim Gottsmann(Executive Editor)
Short summary
We identified several problems in Urbani et al. (2020), showing that their model does not conform to the age and location of faulting, identification and delimitation of uplifted areas and apical depressions, temperature and lithological well log, and stratigraphic and radiometric data. Published data indicate that the pressurization of the Los Humeros volcanic complex (LHVC) magmatic–hydrothermal system driving resurgence faulting occurs at a greater depth.