Articles | Volume 13, issue 3
Research article
18 Mar 2022
Research article |  | 18 Mar 2022

Together but separate: decoupled Variscan (late Carboniferous) and Alpine (Late Cretaceous–Paleogene) inversion tectonics in NW Poland

Piotr Krzywiec, Mateusz Kufrasa, Paweł Poprawa, Stanisław Mazur, Małgorzata Koperska, and Piotr Ślemp


Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on se-2021-105', Gabor Tari, 24 Sep 2021
    • AC1: 'Reply on RC1', Piotr Krzywiec, 11 Nov 2021
  • RC2: 'Comment on se-2021-105', Mark Cooper, 07 Oct 2021
    • AC2: 'Reply on RC2', Piotr Krzywiec, 11 Nov 2021

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Piotr Krzywiec on behalf of the Authors (04 Feb 2022)  Author's response    Author's tracked changes    Manuscript
ED: Publish as is (11 Feb 2022) by Jonas Kley
ED: Publish subject to technical corrections (12 Feb 2022) by Susanne Buiter(Executive Editor)
AR by Piotr Krzywiec on behalf of the Authors (13 Feb 2022)  Author's response    Manuscript
Short summary
Legacy 2-D seismic data with newly acquired 3-D seismic data were used to construct a new model of geological evolution of NW Poland over last 400 Myr. It illustrates how the destruction of the Caledonian orogen in the Late Devonian–early Carboniferous led to half-graben formation, how they were inverted in the late Carboniferous, how the study area evolved during the formation of the Permo-Mesozoic Polish Basin and how supra-evaporitic structures were inverted in the Late Cretaceous–Paleogene.