@incollection{gledocs_11858_00-1735-0000-0001-3485-D,
author = {Laukamp, Carsten and Petzel, Volker and Bechstädt, Thilo},
editor = {Philipp, Sonja and Leiss, Bernd and Vollbrecht, Axel and Tanner, David and Gudmundsson, Agust},
title = {Structural control of fluid flow on a carbonate platform margin: an example from the Otavi Mountainland, Namibia},
booktitle = {11. Symposium "Tektonik, Struktur- und Kristallingeologie"},
year = {2006-03},
publisher = {Universitätsverlag Göttingen},

abstract = {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.},
note = { \url {http://hdl.handle.net/11858/00-1735-0000-0001-3485-D}},
}