dc.contributor.author | Laukamp, Carsten | |
dc.contributor.author | Petzel, Volker | |
dc.contributor.author | Bechstädt, Thilo | |
dc.contributor.editor | Philipp, Sonja | |
dc.contributor.editor | Leiss, Bernd | |
dc.contributor.editor | Vollbrecht, Axel | |
dc.contributor.editor | Tanner, David | |
dc.contributor.editor | Gudmundsson, Agust | |
dc.date.accessioned | 2010-11-26T13:21:40Z | |
dc.date.accessioned | 2013-01-28T10:19:51Z | |
dc.date.available | 2010-11-26T13:21:40Z | |
dc.date.available | 2013-01-28T10:19:51Z | |
dc.date.issued | 2006-03 | |
dc.identifier.citation | Philipp, S.; Leiss, B; Vollbrecht, A.; Tanner, D.; Gudmundsson, A. (eds): 11. Symposium "Tektonik, Struktur- und Kristallingeologie"; 2006, Univ.-Verl. Göttingen, p. 125 - 127. | |
dc.identifier.isbn | 3-938616-40-7 | |
dc.identifier.uri | http://hdl.handle.net/11858/00-1735-0000-0001-3485-D | |
dc.description.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. | |
dc.format.mimetype | application/pdf | |
dc.language.iso | deu | |
dc.publisher | Universitätsverlag Göttingen | |
dc.relation.ispartof | 11. Symposium "Tektonik, Struktur- und Kristallingeologie" | |
dc.subject.ddc | 551 | |
dc.subject.gok | VER 200 | |
dc.subject.gok | VAE 400 | |
dc.subject.gok | VAE 814 | |
dc.subject.gok | VQD 200 | |
dc.subject.gok | VKB 294 | |
dc.title | Structural control of fluid flow on a carbonate platform margin: an example from the Otavi Mountainland, Namibia | |
dc.type | anthologyArticle | |
dc.subject.gokverbal | Namibia {Geologie} | |
dc.subject.gokverbal | Tektogenese {Geologie} | |
dc.subject.gokverbal | Präkambrische Orogene {Geologie} | |
dc.subject.gokverbal | Metamorphe Lagerstätten | |
dc.subject.gokverbal | Metamorphe Komplexe, Afrika {Petrologie} | |
dc.bibliographicCitation.firstPage | 125 | |
dc.bibliographicCitation.lastPage | 127 | |
dc.identifier.doi | 10.23689/fidgeo-1849 | |
dc.type.version | publishedVersion | |
dc.subject.free | Damara Orogen | |
dc.subject.free | Otavi-Bergland | |
dc.subject.free | Carbonatplattform | |
dc.subject.free | Tektogenese | |
dc.subject.free | Hydrothermale Phase | |
dc.relation.collection | Geologische Wissenschaften | |
dc.description.type | conference | |