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 | EF: Editorial file upload
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.