Articles | Volume 12, issue 8
Solid Earth, 12, 1899–1930, 2021
https://doi.org/10.5194/se-12-1899-2021
Solid Earth, 12, 1899–1930, 2021
https://doi.org/10.5194/se-12-1899-2021

Research article 20 Aug 2021

Research article | 20 Aug 2021

Thermal history of the East European Platform margin in Poland based on apatite and zircon low-temperature thermochronology

Dariusz Botor 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-2021-8', Anonymous Referee #1, 05 Mar 2021
    • AC1: 'Reply on RC1', Dariusz Botor, 31 Mar 2021
  • RC2: 'Comment on se-2021-8', Anonymous Referee #2, 30 Mar 2021
    • AC2: 'Reply on RC2', Dariusz Botor, 02 Jun 2021

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Dariusz Botor on behalf of the Authors (25 Jun 2021)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (29 Jun 2021) by Patrice Rey
RR by Anonymous Referee #1 (04 Jul 2021)
ED: Publish as is (09 Jul 2021) by Patrice Rey
ED: Publish as is (09 Jul 2021) by Joachim Gottsmann(Executive Editor)
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Short summary
The thermal evolution of the East European Platform is reconstructed by means of thermal maturity and low-temperature thermochronometry. Results showed that major heating occurred before the Permian, with maximum paleotemperatures in the earliest and latest Carboniferous for Baltic–Podlasie and Lublin basins, respectively. The Mesozoic thermal history was characterized by gradual cooling from peak temperatures at the transition from Triassic to Jurassic due to decreasing heat flow.