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Vingerbreek Shale

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Journal Article
Published: 01 January 2009
Journal of Paleontology (2009) 83 (1): 110-122.
... of the Nudaus Formation, and in the Feldschuhhorn Member of the overlying Urisis Formation. These shale members constitute outer shelf facies, formed during transgressive backstepping of coarser shelf sandstone units ( Grotzinger and Miller, 2008 ). The Vingerbreek Member consists of green mudstone...
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Journal Article
Published: 01 December 2008
South African Journal of Geology (2008) 111 (4): 357-368.
... shale locally containing turbiditic Schwarzrand successions ( e.g. the Vingerbreek Member, Schwarzrand Subgroup, Nama Group) that end in reddish sediments ( e.g. the Fish River Subgroup, Nama Group) ( Germs, 1995 ) (Figure 7 ). The Cango Caves Group shows a similar trend, clastics and carbonates near...
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Journal Article
Published: 01 March 2012
South African Journal of Geology (2012) 115 (1): 91-102.
... in southern Africa the Vingerbreek Unconformity was formed. This unconformity has been named after the late Ediacaran, shale-rich lower Vingerbreek Member (Nudaus Formation, Schwarzrand Subgroup), in which the unconformity occurs in the Klein Karas Mountains. ( Germs, 1972 ; 1995 ; Figures 2 and 3...
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Journal Article
Published: 01 December 2018
South African Journal of Geology (2018) 121 (4): 451-462.
.... The dominantly carbonate-shale and clastic turbidite successions of the late Neoproterozoic Cango Caves Group have been studied in the past. The first study of the CCG (previously named Cango Series) was carried out by Dunn in 1887, followed by Carstophine and Rogers (1897), Rogers and Schwarz (1900) , Wybergh...
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Journal Article
Journal: PALAIOS
Published: 01 December 2002
PALAIOS (2002) 17 (6): 533-544.
... understand the conditions under which microbial mats form and those under which they become preserved as wrinkle structures. Society for Sedimentary Geology 2002 Above these basal beds follow thinly laminated sandy shales that give the succession a homogeneous appearance. Only a few, 2-to-10-cm...
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Series: Geological Society, London, Special Publications
Published: 01 January 2009
DOI: 10.1144/SP326.16
EISBN: 9781862395749
... ; de Almeida et al. 1976 ; de Brito Neves & Cordani 1991 ). The presence of limestones and organic-rich shales within these sedimentary sequences could suggest the existence of petroleum systems, but which, owing to the limited existing data, have been rarely studied. The purpose of this paper...
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Journal Article
Published: 01 January 2012
Journal of Paleontology (2012) 86 (1): 7-18.
... for Ediacaran undermat miners are the structures illustrated in the Vingerbreek Member of the Nudaus Formation of Namibia by Bouougri and Porada (2007) , which await further description. An early Cambrian shallow-marine (upper offshore to offshore transition) ichnofauna is documented from...
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Journal Article
Journal: PALAIOS
Published: 01 February 2008
PALAIOS (2008) 23 (2): 65-77.
... of sandstone or siltstone layers. These layers usually form distinct beds in successions of finer-grained sediments, frequently shales (e.g., McKee, 1954 ; Martinsson, 1965 ; Häntzschel and Reineck, 1968 ; Bloos, 1976 ; Pflüger, 1999 ; Noffke, 2000 ; Gingras, 2002 ; Noffke et al., 2002 , 2003b...
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