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Tviberg

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Journal Article
Published: 01 September 1996
Geological Magazine (1996) 133 (5): 573-582.
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(A) Rare earth element (REE) and (B) mid-ocean-ridge basalt (MORB)–normaliz...
Published: 01 July 2012
Figure 9. (A) Rare earth element (REE) and (B) mid-ocean-ridge basalt (MORB)–normalized multi-element patterns of dikes and gabbro from Tviberg (Solund-Stavfjord ophiolite complex). Location: See Figures 1 and 2 .
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Sketch map showing the inferred distribution of the three structural domain...
Published: 01 July 2012
Figure 4. Sketch map showing the inferred distribution of the three structural domains of the Solund-Stavfjord ophiolite complex (SSOC), and representative field pictures. (A) Basaltic dike complex intruded by light-gray to white quartz diorite (location: western part of Tviberg; Fig. 2 ). (B
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Simplified geological map of the Solund-Bremanger area showing the stratigr...
Published: 01 July 2012
are: Sogneskollen—434 Ma ( Hacker et al., 2003 ); Hersvik—439 Ma ( Hartz et al., 2002 ); Tviberg—443 Ma ( Dunning and Pedersen, 1988 ); Gåsøy—443 Ma, and Bremanger—440 Ma ( Hansen et al., 2002 ).
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Harker variation diagrams for related granitic rocks in Hyllestad, Stavfjor...
Published: 01 November 2000
Fig. 9. Harker variation diagrams for related granitic rocks in Hyllestad, Stavfjord and Lindås. Filled circles: Sogneskollen granodiorite; filled squares: Sogneskollen biotite-granite dykes; open triangles: minor granitic sheets from Tviberg; filled diamondås: granitic sheets from Svanøy; open
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Harker variation diagrams for related granitic rocks in Hyllestad, Stavfjor...
Published: 01 November 2000
Fig. 9. Harker variation diagrams for related granitic rocks in Hyllestad, Stavfjord and Lindås. Filled circles: Sogneskollen granodiorite; filled squares: Sogneskollen biotite-granite dykes; open triangles: minor granitic sheets from Tviberg; filled diamondås: granitic sheets from Svanøy; open
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Cartoon showing the formation and obduction of the Solund–Stavfjord Ophioli...
Published: 01 November 2000
of a transform fault is indicated by the field relationships on the island of Tviberg ( Fig. 1, Skjerlie et al. 1989; Skjerlie & Furnes 1990). Sill intrusions in the cover sediments to the ophiolite complex suggest that very large amounts of sediments (greywacke) accumulated in the basin. The presence
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Cartoon showing the formation and obduction of the Solund–Stavfjord Ophioli...
Published: 01 November 2000
of a transform fault is indicated by the field relationships on the island of Tviberg ( Fig. 1, Skjerlie et al. 1989; Skjerlie & Furnes 1990). Sill intrusions in the cover sediments to the ophiolite complex suggest that very large amounts of sediments (greywacke) accumulated in the basin. The presence
Journal Article
Published: 01 February 1990
Journal of the Geological Society (1990) 147 (1): 59-68.
.... Geologiske relasjoner mellom gabbro og gangkompleks, petrogenese og tektonomagmatisk modellutvikling i området Tviberg-NV. Atløy, Solund-Stavfjorden Ofiolittkompleks. Cand. Scient. thesis. University of Bergen. Skjerlie, K. P., Furnes, H. & Johansen, R. J. 1989. Magmatic development and tectono...
Journal Article
Journal: GSA Bulletin
Published: 01 July 2012
GSA Bulletin (2012) 124 (7-8): 1027-1047.
...Figure 9. (A) Rare earth element (REE) and (B) mid-ocean-ridge basalt (MORB)–normalized multi-element patterns of dikes and gabbro from Tviberg (Solund-Stavfjord ophiolite complex). Location: See Figures 1 and 2 . ...
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Journal Article
Published: 01 November 2000
Journal of the Geological Society (2000) 157 (6): 1199-1213.
...Fig. 9. Harker variation diagrams for related granitic rocks in Hyllestad, Stavfjord and Lindås. Filled circles: Sogneskollen granodiorite; filled squares: Sogneskollen biotite-granite dykes; open triangles: minor granitic sheets from Tviberg; filled diamondås: granitic sheets from Svanøy; open...
FIGURES | View All (9)
Journal Article
Published: 01 August 2013
Petroleum Geoscience (2013) 19 (3): 289-304.
... developed in the Petroleum Geology class at NTNU, Trondheim, Norway ( Tviberg 2011 ). The controlled basin environment is called the Bezurk Basin ( Fig. 1 ), and it includes three potential kinds of prospects, namely anticlinal type, fault type and a shoestring type. The latter is located within impermeable...
FIGURES | View All (17)
Series: GSA Field Guide
Published: 01 January 2011
DOI: 10.1130/2011.FLD019.21
EISBN: 9780813756196
... excursion on the western shore of lake Sjøralden, inspecting fluvial conglomerates of the Sjøralden Formation (Herland Group) and the well-exposed unconformity above the Høyvik Group. (D) View from Brurestakken toward the islands Alden and Tviberg in the west (see also Fig. 34E ). The islands are composed...
Series: Geological Society, London, Special Publications
Published: 01 January 2003
DOI: 10.1144/GSL.SP.2003.218.01.20
EISBN: 9781862394667
... defined by its dyke swarms and sheeted dyke complex. Domain II, which represents the oldest crust, contains a NW-trending sheeted dyke complex and high-level gabbros. Where Domains I and II approach each other on Tviberg ( Fig. 1 b), the dykes of Domain II curve from a NW direction to an ENE direction...
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