%0 Conference Paper %A Laukamp, Carsten %A Petzel, Volker %A Bechstädt, Thilo %E Philipp, Sonja %E Leiss, Bernd %E Vollbrecht, Axel %E Tanner, David %E Gudmundsson, Agust %T Structural control of fluid flow on a carbonate platform margin: an example from the Otavi Mountainland, Namibia %B 11. Symposium "Tektonik, Struktur- und Kristallingeologie" %D 2006 %R 10.23689/fidgeo-1849 %I Universitätsverlag Göttingen %X The present study focuses on the northwestern OML, southwest of the mining town of Tsumeb. The dominating structure in this area is the NW-SE striking Guinas Fault. The Guinas Fault is a shear zone that divides an area, which is different in sense of stratigraphic features, the grade of pre-, syn- and post- Damaran deformation and the type and grade of mineralisation. The northern area is enriched by Cu-rich base metal sulphides, whereas the southern area is almost barren. %U http://hdl.handle.net/11858/00-1735-0000-0001-3485-D %~ FID GEO-LEO e-docs