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Ombonde Detachment

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Journal Article
Journal: Geology
Published: 01 August 1999
Geology (1999) 27 (8): 687-690.
...Paul F. Hoffman; Ebbe H. Hartz Abstract The Ombonde detachment is a primary low-angle normal fault that developed in an undeformed Neoproterozoic carbonate shelf succession as it entered a west-dipping Pan-African subduction zone. The fault is mappable from the top of the shelf succession...
Journal Article
Published: 19 January 2016
Canadian Journal of Earth Sciences (2016) 53 (11): 1177-1189.
... indicates the steep frontal ramp in B, not the toe of the detachment. [Colour online.] The discovery of the Ombonde detachment ( Hoffman and Hartz 1999 ) in the Kaoko belt of Namibia ( Fig. 2 ) provided an Ediacaran example for which the net displacement, paleotectonic setting, and longitudinal (i.e...
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Image
(A) Geologic map of the Grootberg syncline (location,  Fig. 3 ). Red line i...
Published: 19 January 2016
Fig. 5. (A) Geologic map of the Grootberg syncline (location, Fig. 3 ). Red line is the Ombonde detachment (ticks on hangingwall), a brittle, low-angle, normal-sense detachment that ramps stratigraphically downward from east to west and omits ∼400 m of stratigraphic section at any location
Image
Tectonic map of northwest Namibia showing elements of the Congo and Kalahar...
Published: 19 January 2016
Fig. 3. Tectonic map of northwest Namibia showing elements of the Congo and Kalahari cratons, and the Kaoko and Damara orogenic belts (adapted from Hoffmann 1987 ). Boxes in the Eastern Kaoko zone (EKz) frame the Ombonde ( Fig. 5 ) and Ombepera ( Fig. 6 ) detachment areas. Dashed magenta line
Journal Article
Journal: GSA Bulletin
Published: 01 June 2000
GSA Bulletin (2000) 112 (6): 871-883.
..., California : Tectonics , v. 8 p. 453 - 467 . Hoffman , P.F. , 1998 , Ombonde detachment, Namibia: A primary low-angle normal fault associated with foreland flexure : Geological Society of America Abstracts with Programs , v. 30 p. 20 . Holm , D.K. , and Wernicke , B.P. , 1990...
FIGURES | View All (17)