Scheduled Cruises in 2005
Summary of a cruise on margins research (D.051)
Agulhas Bank - Agulhas Plateau - Transkei Basin 34 S/21 E - 43 S/ 35
E (S South Africa)
RV Sonne So-182
4th April 2005 from : Cape Town, South Africa
18th May 2005 in : Cape Town, South Africa
44 days
Gabriele
Uenzelmann-Neben
Alfred-Wegener-Institute for Polar and Marine Research (AWI)
K. Gohl (AWI)
Structure and Dynamics of the Lithosphere and Polar Ice Sheets - here
The oceanic plateaux and basin offshore South Africa play a major role
in understanding the tectono-geodynamic
evolution since the break-up of Gondwana and the development of ocean
currents in the southern Atlantic
and Indian Ocean.
We intend to investigate the development of basins, plateaux and ridges
such as Agulhas Plateau and Mozambique
Ridge as well as the accompanying magmatism active during the opening
of the Southern Ocean, and the
correlation between volcano-tectonic activities of plateaux, basins and
the Agulhas Falkland Fracture Zone
(AFFZ) and the changing deep sea currents.
We will gather seismic refraction/wide angle data along a geophysical
transect from South Africa across the
AFFZ and the Agulhas Plateau into the basin southwest of the plateau to
learn about the geodynamic processes
and plate tectonic evolution of this area since the Cretaceous.
High resolution seismic reflection data will be gathered on the Agulhas
Plateau and in the Transkei Basin to
reconstruct the evolution and modification in oceanic currents and heat
transport since the opening of the gateway.
Image extracted from the GEBCO
Digital Atlas published by the
British Oceanographic Data Centre
on behalf of IOC and IHO, 2003.
Fig - Agulhas Plateau & Transkei Basin
(off South Africa).
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