Articles | Volume 11, issue 2
https://doi.org/10.5194/se-11-527-2020
https://doi.org/10.5194/se-11-527-2020
Research article
 | 
16 Apr 2020
Research article |  | 16 Apr 2020

Estimating the depth and evolution of intrusions at resurgent calderas: Los Humeros (Mexico)

Stefano Urbani, Guido Giordano, Federico Lucci, Federico Rossetti, Valerio Acocella, and Gerardo Carrasco-Núñez

Download

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Stefano Urbani on behalf of the Authors (08 Oct 2019)  Author's response   Manuscript 
ED: Publish subject to technical corrections (15 Oct 2019) by Johan Lissenberg
ED: Publish subject to minor revisions (review by editor) (02 Dec 2019) by Johan Lissenberg
AR by Stefano Urbani on behalf of the Authors (04 Dec 2019)  Author's response   Manuscript 
ED: Publish subject to minor revisions (review by editor) (11 Dec 2019) by Johan Lissenberg
AR by Stefano Urbani on behalf of the Authors (11 Dec 2019)  Author's response   Manuscript 
ED: Publish as is (08 Jan 2020) by Johan Lissenberg
ED: Publish as is (12 Jan 2020) by Joachim Gottsmann (Executive editor)
AR by Stefano Urbani on behalf of the Authors (13 Jan 2020)

Post-review adjustments

AA: Author's adjustment | EA: Editor approval
AA by Stefano Urbani on behalf of the Authors (08 Apr 2020)   Author's adjustment   Manuscript
EA: Adjustments approved (09 Apr 2020) by Johan Lissenberg
Download
Short summary
In Los Humeros, through field structural–geological mapping and analogue experiments, we show a discontinuous and small-scale (areal size ~ 1 km2) uplift of the caldera floor due to the emplacement of multiple shallow (< 1 km) magmatic bodies. These results allow for a better assessment of the subsurface structure of Los Humeros, with crucial implications for planning future geothermal exploration, which should account for the local geothermal gradient affected by such a shallow heat source.