Articles | Volume 13, issue 2
Solid Earth, 13, 431–448, 2022
https://doi.org/10.5194/se-13-431-2022
Solid Earth, 13, 431–448, 2022
https://doi.org/10.5194/se-13-431-2022

Research article 02 Mar 2022

Research article | 02 Mar 2022

Crustal structure of the Volgo–Uralian subcraton revealed by inverse and forward gravity modelling

Igor Ognev et al.

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on se-2021-98', Anonymous Referee #1, 11 Sep 2021
    • AC1: 'Reply on RC1', Igor Ognev, 17 Nov 2021
  • RC2: 'Comment on se-2021-98', Anonymous Referee #2, 12 Oct 2021
    • AC2: 'Reply on RC2', Igor Ognev, 17 Nov 2021
    • AC3: 'Reply on RC2', Igor Ognev, 21 Nov 2021

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Igor Ognev on behalf of the Authors (21 Nov 2021)  Author's response    Author's tracked changes    Manuscript
ED: Publish as is (23 Nov 2021) by Nicolas Gillet
ED: Referee Nomination & Report Request started (02 Dec 2021) by Susanne Buiter
RR by Anonymous Referee #1 (28 Dec 2021)
RR by Anonymous Referee #2 (17 Jan 2022)
ED: Publish subject to minor revisions (review by editor) (18 Jan 2022) by Susanne Buiter
AR by Igor Ognev on behalf of the Authors (22 Jan 2022)  Author's response    Author's tracked changes    Manuscript
ED: Publish as is (24 Jan 2022) by Susanne Buiter
ED: Publish as is (24 Jan 2022) by Susanne Buiter(Executive Editor)
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Short summary
We present a new 3D crustal model of Volgo–Uralia, an eastern segment of the East European craton. We built this model by processing the satellite gravity data and using prior crustal thickness estimation from regional seismic studies to constrain the results. The modelling revealed a high-density body on the top of the mantle and otherwise reflected the main known features of the Volgo–Uralian crustal architecture. We plan to use the obtained model for further geothermal analysis of the region.