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Sundvollen Formation

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FIGURE 7 —Suspected microbial mat impressions, <span class="search-highlight">Sundvollen</span> <span class="search-highlight">Formation</span>, Ringer...
Published: 01 February 2006
FIGURE 7 —Suspected microbial mat impressions, Sundvollen Formation, Ringerike. Black bar = 1-cm scale. (A) Contrasting red and drab siltstones suggesting restricted oxidization conditions; crinkled lamina that separates the two horizons is calcareous, and the bedding plane it represents displayed
Journal Article
Journal: PALAIOS
Published: 01 February 2006
PALAIOS (2006) 21 (1): 46–62.
...FIGURE 7 —Suspected microbial mat impressions, Sundvollen Formation, Ringerike. Black bar = 1-cm scale. (A) Contrasting red and drab siltstones suggesting restricted oxidization conditions; crinkled lamina that separates the two horizons is calcareous, and the bedding plane it represents displayed...
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FIGURE 3 —Repichnial trace fossils from the Ringerike Group. Black bar in e...
Published: 01 February 2006
FIGURE 3 —Repichnial trace fossils from the Ringerike Group. Black bar in each image except E = 1-cm scale. (A) Cruziana isp. (Form A), Sundvollen Formation, Ringerike. (B) “ Merostomichnites ,” Sundvollen Formation, Ringerike (Paleontologisk Museum, Oslo [PMO] No. 98124). (C) Siskemia
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FIGURE 5 —Examples of ? Polarichnus garnierensis  from the <span class="search-highlight">Sundvollen</span> Forma...
Published: 01 February 2006
FIGURE 5 —Examples of ? Polarichnus garnierensis from the Sundvollen Formation, Ringerike. Black bar = 1-cm scale. (A) Giant Polarichnus -type trace; Sundvollen Formation, Ringerike, visible ruler is 40 cm. (B) Superimposed ? Polarichnus traces (PMO No. 97135); Sundvollen Formation, Ringerike
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FIGURE 4 —Selected trace fossils from the Ringerike Group. Black bar = 1-cm...
Published: 01 February 2006
FIGURE 4 —Selected trace fossils from the Ringerike Group. Black bar = 1-cm scale. (A) Didymaulichnus isp., Holmestrand Formation, Jeløya. (B) Margaritichnus isp., Holmestrand Formation, Løvøya, Holmestrand. (C) Fugichnial escape structures, Sundvollen Formation (calcarenite horizon), Ringerike
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FIGURE 8 —Examples of sedimentary logs from the Ringerike Group showing the...
Published: 01 February 2006
FIGURE 8 —Examples of sedimentary logs from the Ringerike Group showing the position of trace-fossil associations (not including Association E) within the coastal successions. (A) Sedimentary logs of the Sundvollen Formation at Ringerike. (B) Sedimentary logs of the Holmestrand Formation at Jeløya
Journal Article
Published: 29 October 2013
Geological Magazine (2014) 151 (5): 816–829.
... with the deposition of the carbonates of the Steinsfjorden Formation ( Fig. 2 ). A transition to non-marine and red-bed facies (Sundvollen Formation) occurred at or just below the Wenlock–Ludlow boundary (Bruton, Gabrielsen & Larsen, 2010 ). The Old Red Sandstone sediments of the Late...
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Journal Article
Published: 30 April 2015
Journal of the Geological Society (2015) 172 (4): 465–478.
... recycling of older units has been suggested ( Kristoffersen et al . 2014 ). The transition from marine to non-marine conditions at the Wenlock–Ludlow boundary is recorded by the deposition of the Old Red Sandstone of the Ringerike Group (Sundvollen Formation). It marks an abrupt change in the tectonic...
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Journal Article
Published: 01 April 2008
Earth Sciences History (2008) 27 (1): 31–58.
... of stratigraphic position and lithological similarity to the Old Red Sandstone of Scotland. Additional work has subsequently subdivided these red beds into two formations, the Sundvollen Formation overlain by the Stubbdal Formation ( Turner 1974 ). The Sundvollen Formation is interpreted as the product...
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Journal Article
Published: 01 June 2009
Scottish Journal of Geology (2009) 45 (1): 83–87.
... shelf Narbonne (1984) Gordia marina Lower Sundvollen Formation, Norway (Upper Silurian) Broad coastal plain; marginal marine Davies et al . (2006) ...
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Journal Article
Journal: Geology
Published: 01 January 2010
Geology (2010) 38 (1): 51–54.
...-Devonian successions (Cotter's Silurian meandering examples, the Bloomsburg and Sundvollen Formations, have been reinterpreted as muddy coastal-plain facies; Driese et al., 1992 ; Davies et al., 2006 ). Figure 1 suggests an absence of meandering fluvial systems prior to the Ludlow, with the number...
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Journal Article
Published: 01 August 1994
Journal of the Geological Society (1994) 151 (4): 669–680.
... similar. When their horizons are broadly correlated, the Semsvik band is placed in the upper Virgilian Stage of the upper Pennsylvanian and in the upper Stephanian C of Europe. This age, which is applicable to the thin succession of the Asker Group in general, pre-dates formation of the Oslo Graben...
Journal Article
Journal: PALAIOS
Published: 29 December 2022
PALAIOS (2022) 37 (12): 731–743.
... Silurian coastal settings: Gariwerdichnus warreni from the Major Mitchell Sandstone of Australia ( Gouramanis et al. 2021 ), and Polarichnus garnierensis from the Sundvollen Formation of Norway ( Davies et al. 2006 ), which reached maximum diameters of 200 mm and 185 mm respectively. Other than a few...
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Series: SEPM Concepts in Sedimentology and Paleontology
Published: 01 January 2013
DOI: 10.2110/sepmcsp.11.047
EISBN: 9781565762893
... (“cornstone”) nature of the carbonate nodules and lumps from the Late Wenlock Sundvollen Formation of the Ringerike (CA48: 60°N, 11°E) area. Bryhni (1978) described some Old Red Sandstone type sediments, with what sounds like calcrete, from the Hornelen Basin (CA49: 62°N, 5.5°E) of western Norway...
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Series: Geological Society, London, Special Publications
Published: 13 January 2021
DOI: 10.1144/SP503-2020-79
EISBN: 9781786209917
... by subsequent work by Slama and Pedersen (2015) . The Sælabonn, Bruflat, Stubdal and Sundvollen Formations are four other clastic units of Silurian age in the Oslo region, all interpreted to have been deposited in a foreland basin SE of the emerging Caledonian orogen to the NW ( Larsen and Olaussen 2005...
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Journal Article
Published: 13 April 2020
Geological Magazine (2020) 157 (12): 1939–1970.
... (e.g. the Sundvollen Formation, Norway (Davies et al. 2006 )) transitional environments. There is an apparent global dip in ichnodiversity and ichnodisparity in marine and transitional strata of Devonian age (such as those typified by the Catskill complex of the NE United States (Miller, 1979 ; Knox...
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