Imaging the East European Craton margin in northern Poland using extended correlation processing of regional seismic reflection profiles

Mężyk, Miłosz; Malinowski, Michał; Mazur, Stanisław

doi:https://doi.org/10.5194/se-10-683-2019

Articles | Volume 10, issue 3

https://doi.org/10.5194/se-10-683-2019

© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.

Special issue:

Advances in seismic imaging across the scales

https://doi.org/10.5194/se-10-683-2019

© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 10, issue 3

Research article

|

21 May 2019

Research article |

| 21 May 2019

Imaging the East European Craton margin in northern Poland using extended correlation processing of regional seismic reflection profiles

Miłosz Mężyk, Michał Malinowski, and Stanisław Mazur

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Final revised paper (published on 21 May 2019)
Preprint (discussion started on 21 Feb 2019)

Interactive discussion

Status: closed

AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

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RC1: 'Review: Imaging East European Craton margin in Northern Poland using extended-correlation processing applied to regional reflection seismic profiles', Anonymous Referee #1, 08 Mar 2019
- AC1: 'Reply to Referee 1', Milosz Mezyk, 20 Mar 2019
RC2: 'Review of Mezyk et al.', Anonymous Referee #2, 09 Mar 2019
- AC2: 'Reply to Referee 2', Milosz Mezyk, 20 Mar 2019

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision

AR by Milosz Mezyk on behalf of the Authors (09 Apr 2019) Manuscript

ED: Publish as is (21 Apr 2019) by Ramon Carbonell

ED: Publish as is (29 Apr 2019) by CharLotte Krawczyk (Executive editor)

AR by Milosz Mezyk on behalf of the Authors (30 Apr 2019)

Short summary

The Precambrian East European Craton is one of the most important building blocks of the European plate. Unlike in Scandinavia, its crystalline crust in Poland is concealed beneath younger sediments. Reprocessing of ca. 950 km regional reflection seismic profiles acquired during shale gas exploration in NE Poland revealed reflectivity patterns interpreted as signs of Svekofennian orogeny, proving a similar mechanism of Paleoproterozoic crustal formation across the Baltic Sea.