Articles | Volume 16, issue 6
https://doi.org/10.5194/se-16-425-2025
https://doi.org/10.5194/se-16-425-2025
Research article
 | 
06 Jun 2025
Research article |  | 06 Jun 2025

Lithologically constrained velocity–density relationships and vertical stress gradients in the North Alpine Foreland Basin, SE Germany

Peter Obermeier, Florian Duschl, and Michael C. Drews

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • CC1: 'Comment on egusphere-2024-2692', Giacomo Medici, 30 Sep 2024
    • AC3: 'Reply on CC1', Michael Drews, 14 Feb 2025
  • RC1: 'Comment on egusphere-2024-2692', Anonymous Referee #1, 18 Dec 2024
    • AC1: 'Reply on RC1', Michael Drews, 14 Feb 2025
  • RC2: 'Comment on egusphere-2024-2692', Anonymous Referee #2, 19 Dec 2024
    • AC2: 'Reply on RC2', Michael Drews, 14 Feb 2025

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Michael Drews on behalf of the Authors (14 Feb 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (01 Mar 2025) by Florian Fusseis
ED: Publish as is (01 Mar 2025) by Florian Fusseis (Executive editor)
AR by Michael Drews on behalf of the Authors (12 Mar 2025)
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Short summary
We investigate geophysical properties and the distribution of vertical stress, which is defined by the weight of the rock column above a certain location in the subsurface, in the upper 5 km of the North Alpine Foreland Basin in Germany. Our results help us to understand the present-day geological configuration and to improve safety for subsurface use, such as deep geothermal energy production in the study area.
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