Lithospheric structure of the Namibian continental passive margin at the intersection with the Walvis Ridge from amphibious seismic investigations
Passive continental margins offer the unique opportunity to study the processes involved in continental extension and break up and the role of hot-spot related magmatism. A combined on- and offshore seismic experiments was designed to characterize the Southern African passive margin at the location of the Walvis Ridge, to assess the interaction of the presumed plume with continental lithosphere and to determine the deep structure of the transition from the coastal fold belt to the stable craton, where the Walvis Ridge hits the African continent. The project integrates three experiments, (A) an onshore, coast-parallel refraction seismic profile, (B) two onshore-offshore wide-angle seismic transects, and (C) a combined on- and offshore seismic imaging of the sub-Moho velocity (Pn tomography) at the ocean-continent transition. The derived lithospheric structure of the margin together with results from other geoscientific studies (e.g., conducted within the SPP-SAMPLE) will help to address questions such as, how continental crust and plume head interact, what the extent and volumes of magmatic underplating is, and how and which inherited (continental) structures might have been involved and utilized in the break up process.
- 11/2010 - 02/2011 (experiment)
- Trond Ryberg (GFZ Potsdam)
- Christian Haberland (GFZ Potsdam)
- Michael Weber (GFZ Potsdam)
- Jan Behrmann (IfM-Geomar)
- Wilfried Jokat (AWI)
- Klaus Bauer (GFZ Potsdam)
- Geological Survey Namibia
- other groups of SAMPLE
Methods & Equipment
- refraction / wide-angle reflection
- 200 DSS Cubes
- Ryberg, T., Haberland, C. (2021): Data of the controlled source seismic profile LISPWAL2: Lithospheric structure of the Namibian continental passive margin at the intersection with the Walvis Ridge. doi.org/10.5880/GIPP.201111.1
- Fromm, T., Jokat, W., Ryberg, T., Behrmann, J. H., Haberland, C., Weber, M. (2017): The onset of Walvis Ridge: Plume influence at the continental margin. - Tectonophysics, 716, 90-107.
- Ryberg, T., Braeuer, B., Weber, M. (2016): Upper mantle structure at Walvis Ridge from Pn tomography, Tectonophysics, doi.org/10.1016/j.tecto.2016.08.009
- Ryberg, T., Haberland, C., Haberlau, T., Weber, M., Bauer, K., Behrmann, J. H., Jokat, W. (2015): Crustal structure of northwest Namibia: Evidence for plume-rift-continent interaction, Geology, 43, 8, p. 739-742.