Articles | Volume 13, issue 11
https://doi.org/10.5194/se-13-1755-2022
https://doi.org/10.5194/se-13-1755-2022
Research article
 | 
18 Nov 2022
Research article |  | 18 Nov 2022

Strato-structural evolution of the deep-water Orange Basin: constraints from 3D reflection seismic data

Nombuso G. Maduna, Musa S. D. Manzi, Zubair Jinnah, and Julie E. Bourdeau

Download

Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2022-180', Anonymous Referee #1, 02 Jun 2022
    • RC3: 'Reply on RC1', Chris Elders, 10 Jun 2022
      • RC4: 'Reply on RC3', Anonymous Referee #1, 10 Jun 2022
        • AC6: 'Reply on RC4', Nombuso Maduna, 17 Sep 2022
      • AC3: 'Reply on RC3', Nombuso Maduna, 17 Sep 2022
    • AC2: 'Reply on RC1', Nombuso Maduna, 21 Jun 2022
  • RC2: 'Comment on egusphere-2022-180', Chris Elders, 10 Jun 2022
    • AC1: 'Reply on RC2', Nombuso Maduna, 21 Jun 2022
    • AC4: 'Reply on RC2', Nombuso Maduna, 17 Sep 2022
  • EC1: 'Comment on egusphere-2022-180', CharLotte Krawczyk, 22 Jun 2022
  • RC5: 'Comment on egusphere-2022-180', Anonymous Referee #3, 14 Aug 2022
    • AC5: 'Reply on RC5', Nombuso Maduna, 17 Sep 2022

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Nombuso Maduna on behalf of the Authors (14 Oct 2022)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (14 Oct 2022) by CharLotte Krawczyk
RR by Anonymous Referee #3 (17 Oct 2022)
ED: Publish as is (24 Oct 2022) by CharLotte Krawczyk
ED: Publish as is (24 Oct 2022) by CharLotte Krawczyk (Executive editor)
AR by Nombuso Maduna on behalf of the Authors (26 Oct 2022)
Download
Short summary
High-resolution 3D reflection seismic data from the Orange Basin, South Africa, are used to provide an in-depth examination of features within the Late Cretaceous to Cenozoic sedimentary successions. The study provides insight into the structural styles between the translational and compressional domains of a Late Cretaceous deep-water fold-and-thrust belt (DWFTB) system, together with the tectonic and oceanographic processes responsible for mass-scale erosion in the Cenozoic.