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Structural control of fluid flow on a carbonate platform margin: an example from the Otavi Mountainland, Namibia

Laukamp, Carsten
Petzel, Volker
Bechstädt, Thilo
2006-03
Universitätsverlag Göttingen
Article in Anthology
Verlagsversion
Deutsch
11. Symposium "Tektonik, Struktur- und Kristallingeologie"
DOI: https://doi.org/10.23689/fidgeo-1849
Laukamp, Carsten; Petzel, Volker; Bechstädt, Thilo, 2006-03: Structural control of fluid flow on a carbonate platform margin: an example from the Otavi Mountainland, Namibia. In: Philipp, S.; Leiss, B; Vollbrecht, A.; Tanner, D.; Gudmundsson, A. (eds): 11. Symposium "Tektonik, Struktur- und Kristallingeologie"; 2006, Univ.-Verl. Göttingen, p. 125 - 127., DOI https://doi.org/10.23689/fidgeo-1849.
 
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  • 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.
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  • 11. Symposium "Tektonik, Struktur- und Kristallingeologie" , 2006-03 [74]
Subjects:
Damara Orogen
Otavi-Bergland
Carbonatplattform
Tektogenese
Hydrothermale Phase
Namibia {Geologie}
Tektogenese {Geologie}
Präkambrische Orogene {Geologie}
Metamorphe Lagerstätten
Metamorphe Komplexe, Afrika {Petrologie}
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