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Heuningberg Anticline

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Correlation panel with lithofacies distribution and constraints on the main...
Published: 01 January 2010
Figure 12 Correlation panel with lithofacies distribution and constraints on the main geometric features of Units D/E, E, and F, based on mapping of key surfaces and stratigraphic units, and correlation of a larger number of logs. The panel shows part of the southern flank of the Heuningberg
Journal Article
Published: 01 January 2010
Journal of Sedimentary Research (2010) 80 (1): 97-118.
...Figure 12 Correlation panel with lithofacies distribution and constraints on the main geometric features of Units D/E, E, and F, based on mapping of key surfaces and stratigraphic units, and correlation of a larger number of logs. The panel shows part of the southern flank of the Heuningberg...
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Journal Article
Published: 01 August 2011
Journal of Sedimentary Research (2011) 81 (8): 579-599.
... in detail around a series of east–west-trending folds that plunge gently eastward named the Baviaans syncline (southern study area), the Zoutkloof syncline (central study area), and the Heuningberg anticline (northern study area) ( Fig. 3 ). A key aspect of the study area is that these postdepositional...
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Series: SEPM Special Publication
Published: 01 January 2009
DOI: 10.2110/sepmsp.092.261
EISBN: 9781565762008
..., the structural high separating the Tanqua and Laingsburg sub-basins was proposed to be an eastward extension of the Hexriver Anticline. Fold hingeline diagrams illustrate the noncontinuous nature of the Hexriver, Bontberg, and Heuningberg anticlines ( Fig. 7 ), implying that the structures could not have formed...
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Journal Article
Journal: Geosphere
Published: 01 December 2014
Geosphere (2014) 10 (6): 1076-1093.
... lobe complex ( Morris et al., 2014b ). A second, east-trending system in C3 is present across strike to the north ( Fig. 6C ), supplying clastic material to the Heuningberg anticline area ( Di Celma et al., 2011 ). The lowstand sequence set of the Unit D composite sequence is represented...
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Journal Article
Published: 01 July 2003
Journal of Sedimentary Research (2003) 73 (4): 603-620.
... km ( Fig. 2 ). The antiform with the highest present-day elevation is located in the north of the study area and is known as the Heuningberg Anticline. The shortening recorded by the folds is approximately 10% ( Potts et al. 2000 ). The fold axial surfaces are steeply dipping and strike west-east...
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