Articles | Volume 11, issue 6
https://doi.org/10.5194/se-11-2549-2020
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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AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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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)
AR by Gianluca Norini on behalf of the Authors (20 Nov 2020)  Manuscript 
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.