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

Abstract ∼ ∼ ∼ ∼ ∼  11 Ma, are responsible for the creation and preservation of the extensive slope-parallel channels. This study shows the difference in structural styles of the translational and compressional domains of a Late Cretaceous DWFTB system and the processes responsible for mass-scale erosion in the Cenozoic.

Location
Deutsche Nationalbibliothek Frankfurt am Main
Extent
Online-Ressource
Language
Englisch

Bibliographic citation
Strato-structural evolution of the deep-water Orange Basin: constraints from 3D reflection seismic data ; volume:13 ; number:11 ; year:2022 ; pages:1755-1780 ; extent:26
Solid earth ; 13, Heft 11 (2022), 1755-1780 (gesamt 26)

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

DOI
10.5194/se-13-1755-2022
URN
urn:nbn:de:101:1-2022112404330973737790
Rights
Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
Last update
15.08.2025, 7:31 AM CEST

Data provider

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Associated

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

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