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Tysfjord

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Journal Article
Published: 01 May 2013
European Journal of Mineralogy (2013) 25 (2): 187–191.
...Ritsuro Miyawaki; Kazumi Yokoyama; Tomas A. Husdal Abstract Bastnäsite-(Nd), ideally (Nd,La,Ce)(CO 3 )F, occurs in the Stetind pegmatite, Tysfjord, Nordland, Norway, in association with bastnäsite-(Ce), calcioancylite-(Nd) and/or kozoite-(Nd), stetindite, vyuntspakhkite-(Y) and Y-bearing fluorite...
FIGURES
Journal Article
Published: 01 April 2013
Mineralogical Magazine (2013) 77 (3): 353–366.
...M. A. Cooper; T. A. Husdal; N. A. Ball; Y. A. Abdu; F. C. Hawthorne Abstract Schlüterite-(Y), ideally (Y, REE ) 2 Al(Si 2 O 7 )(OH) 2 F, is a new silicate mineral species from the Stetind pegmatite, Tysfjord, Nordland, Norway. It forms dense, fibrous, radiating aggregates (up to ~2 mm) diverging...
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Journal Article
Journal: GSA Bulletin
Published: 01 January 1988
GSA Bulletin (1988) 100 (1): 140–151.
..., northeast-trending back fold, the Ofoten synform. Within its core are klippen of the structurally highest nappes preserved in this portion of the Caledonides. At Tysfjord, 15 km south of Ofoten, some of the deepest structural levels within the orogen are exposed in the core of the Tysfjord cross-fold...
Image
Cayalsite-(Y) crystal in a cavity of yttrian fluorite from Øvre Lapplægeret, Tysfjord, Northern Norway; width of image 0.2 mm. The crystal drawing in the inset was prepared using VESTA (Momma & Izumi, 2011) (colour online).
Published: 01 August 2015
Fig. 1 Cayalsite-(Y) crystal in a cavity of yttrian fluorite from Øvre Lapplægeret, Tysfjord, Northern Norway; width of image 0.2 mm. The crystal drawing in the inset was prepared using VESTA ( Momma & Izumi, 2011 ) (colour online).
Image
Cayalsite-(Y) crystal in a cavity of yttrian fluorite from Stetind, Tysfjord, Northern Norway. Width of SEM image 1 mm. Indexed crystal faces are shown in the inset. The drawing was prepared using VESTA (Momma & Izumi, 2011). Photograph by Harald Folvik, NHM, Oslo (colour online).
Published: 01 August 2015
Fig. 2 Cayalsite-(Y) crystal in a cavity of yttrian fluorite from Stetind, Tysfjord, Northern Norway. Width of SEM image 1 mm. Indexed crystal faces are shown in the inset. The drawing was prepared using VESTA ( Momma & Izumi, 2011 ). Photograph by Harald Folvik, NHM, Oslo (colour online).
Journal Article
Published: 01 August 2015
European Journal of Mineralogy (2015) 27 (5): 683–694.
...Fig. 1 Cayalsite-(Y) crystal in a cavity of yttrian fluorite from Øvre Lapplægeret, Tysfjord, Northern Norway; width of image 0.2 mm. The crystal drawing in the inset was prepared using VESTA ( Momma & Izumi, 2011 ) (colour online). ...
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Journal Article
Published: 01 January 2014
American Mineralogist (2014) 99 (1): 157–169.
...Paola Bonazzi; Giovanni O. Lepore; Luca Bindi; Christian Chopin; Tomas A. Husdal; Olaf Medenbach Abstract In yttrian fluorite from pegmatites of the Tysfjord granite, Norway, grayish-green to very pale green gatelite-like crystals occur along with millimeter-size aggregates of Y-silicates as a late...
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Journal Article
Published: 01 October 2012
European Journal of Mineralogy (2012) 24 (6): 1053–1060.
...Thomas Malcherek; Boriana Mihailova; Jochen Schlüter; Tomas Husdal Abstract The title mineral has been discovered in a granitic pegmatite at the Stetind quarry, Tysfjord, Norway. Atelisite-(Y) forms pale brown to colourless, transparent crystals of dipyramidally terminated, short-prismatic habit...
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Journal Article
Published: 01 April 2007
Mineralogical Magazine (2007) 71 (2): 179–192.
...G. Raade; O. Johnsen; M. Erambert; O. V. Petersen Abstract Hundholmenite-(Y) occurs as pale brown, subhedral crystals up to 1 mm across, embedded in REE -bearing fluorite, in a granitic pegmatite at Hundholmen, Tysfjord, Nordland County, north Norway. Two other occurrences in the same area...
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Image
SEM-BSE images showing minute lamellae of törnebohmite-(Ce) (light grey, black arrow) intergrown with lamellae of a member of the perbøeite-(Ce)–alnaperbøeite-(Ce) solid solution (dark grey, red arrow) in the samples from Stetind (Tysfjord, Norway). Intermediate grey lamellae likely correspond to intergrowths of thinner lamellae. The image at the top shows the mineral association (hu = hundholmenite-(Y); tö = törnebohmite-(Ce); fl = Y-rich fluorite).
Published: 01 January 2019
Fig. 4 SEM-BSE images showing minute lamellae of törnebohmite-(Ce) (light grey, black arrow) intergrown with lamellae of a member of the perbøeite-(Ce)–alnaperbøeite-(Ce) solid solution (dark grey, red arrow) in the samples from Stetind (Tysfjord, Norway). Intermediate grey lamellae likely
Image
Simplified geologic map of Europe with locations of major pegmatite provinces and fields. Pegmatite provinces (see also Table 6): 1 = Kolmozero-Voronja, Kola, 2 = Northern Karelia, 3 = Bothnian Basin, 4 = Somero-Tammela, 5 = Kaustinen, 6 = Ukrainian Shield, 7 = Tysfjord, 8 = Wiborg-rapakivi granite-related pegmatites, 9 = South Scandinavian, 10 = MeloyGlomfjord, 11 = Leinster, 12 = Góry Sowie, 13 = Dolní Bory-Hate, 14 = Hagendorf-Pleystein, 15 = Strzegom, 16 = Central Iberian zone and Galicia-Trás-Os-Montes zone, 17 = Massif Central, 18 = Alabashka, Central Urals, 19 = Austroalpine unit, 20 = Elba. Abbreviations: DPA = direct products of anatexis, LCT = lithium-cesium-tantalum, NYF = niobium-yttriumfluorine, RMG = residual melts of granitic magmatism.
Published: 01 May 2025
Fig. 4. Simplified geologic map of Europe with locations of major pegmatite provinces and fields. Pegmatite provinces (see also Table 6 ): 1 = Kolmozero-Voronja, Kola, 2 = Northern Karelia, 3 = Bothnian Basin, 4 = Somero-Tammela, 5 = Kaustinen, 6 = Ukrainian Shield, 7 = Tysfjord, 8 = Wiborg
Image
Diffraction conditions for SDF-TEM imaging as applied to the Nyseter (NYS), Sta. Eulalia (EUL), and Tysfjord (TYS) samples. The specimens are tilted from the [210]4H zone axis such that diffracted intensity is in the (00l) lattice row. The dashed circle represents the diameter of the objective aperture used for imaging, centered on the (0040)4H reflection of the substructure. In non-integral NC-pyrrhotites this reflection is weak or extinct, but occasionally occurs due to 4C domains within the diffracting volume.
Published: 01 May 2011
F igure 6. Diffraction conditions for SDF-TEM imaging as applied to the Nyseter (NYS), Sta. Eulalia (EUL), and Tysfjord (TYS) samples. The specimens are tilted from the [210] 4H zone axis such that diffracted intensity is in the (00 l ) lattice row. The dashed circle represents the diameter
Journal Article
Published: 01 January 2019
European Journal of Mineralogy (2019) 31 (1): 173–181.
...Fig. 4 SEM-BSE images showing minute lamellae of törnebohmite-(Ce) (light grey, black arrow) intergrown with lamellae of a member of the perbøeite-(Ce)–alnaperbøeite-(Ce) solid solution (dark grey, red arrow) in the samples from Stetind (Tysfjord, Norway). Intermediate grey lamellae likely...
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Journal Article
Published: 01 July 1973
Journal of the Geological Society (1973) 129 (4): 365–386.
... Foslie S. Tysfjords geologi Norg. geol. Unders 1941 149 Gustavson M. The Caledonian mountain chain of the southern Troms and Ofoten areas.Part 1. Basement rocks and Caledonian metasediments Norg. geol. Unders 1966 239 Haller J. Kulp J. L. Absolute age determinations...
Journal Article
Published: 01 July 2009
The Journal of Geology (2009) 117 (4): 399–414.
...-facies Caledonian nappes that overlie (2) Archean-Proterozoic para- and orthogneisses and granitic plutons of the Tysfjord basement in the east and (3) Archean-Proterozoic mangerites, charnockites, gabbros, and supracrustals of the Lofoten basement in the west. The nappes have been lithologically...
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Journal Article
Journal: Economic Geology
Published: 01 May 2025
Economic Geology (2025) 120 (3): 745–778.
...Fig. 4. Simplified geologic map of Europe with locations of major pegmatite provinces and fields. Pegmatite provinces (see also Table 6 ): 1 = Kolmozero-Voronja, Kola, 2 = Northern Karelia, 3 = Bothnian Basin, 4 = Somero-Tammela, 5 = Kaustinen, 6 = Ukrainian Shield, 7 = Tysfjord, 8 = Wiborg...
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Image
SEM-BSE images of the studied pyrrhotites. (a) Sta. Eulalia (EUL) showing two sets of dark exsolution lamellae of 4C-pyrrhotite in a matrix of NC-pyrrhotite. Adjacent dark areas are also 4C-pyrrhotite. (b) Nyseter (NYS) displaying two sets of dark 4C-pyrrhotite exsolution lamellae in NC matrix. (c) Tysfjord (TYS) displaying a single set of bright troilite (2C-pyrrhotite) exsolution lamellae parallel to (001). Faint lines and striations in (a–c) are artifacts from polishing and high detector gain. (d) Accumulated BSE image of TYS and extracted intensity profile showing dark haloes around troilite lamellae. Although the spatial extent of the BSE generating region causes a considerable convolution of the image, a clear low in backscattered intensity is visible around the lamella, pointing to an approximately 1 μm wide Fe depleted diffusion zone.
Published: 01 May 2011
lamellae in NC matrix. ( c ) Tysfjord (TYS) displaying a single set of bright troilite (2C-pyrrhotite) exsolution lamellae parallel to (001). Faint lines and striations in ( a – c ) are artifacts from polishing and high detector gain. ( d ) Accumulated BSE image of TYS and extracted intensity profile
Journal Article
Published: 01 June 1980
Journal of the Geological Society (1980) 137 (3): 261–270.
.... The motion of thrust sheets J. geophys. Res. 1976 81 949 63 Foslie S. Tysfjords geologi Nor. geol. Unders 1941 149 298 Foslie S. Strand T. Namnsvatnet med en del av Fröyningsfjell Nor. geol. Unders 1956 196 82 Gee D. A tectonic model for the central part...
Journal Article
Published: 01 December 1978
Journal of the Geological Society (1978) 135 (6): 629–647.
... studies Tectonophysics 1976 30 269 98 Foslie S. Tysfjords geologi Norg geol Unders 1941 149 1 298 Glassley W. E. High grade regional metamorphism of some carbonate bodies: Significance for the orthopyroxene isograd Am J Sci 1975 275 1133 63 Green T. H...
Image
fig. 1.Streblacantha circumtexta (Jørgensen, 1900): a, b, lectotype, PMO224.463, slide #52 (O37/2), Tysfjord 28 March 1899, 0–700 m. fig. 2.Streblacantha circumtexta (Jørgensen, 1900). Original drawing of Jørgensen (1900, pl. 11, fig. 46a). fig. 3.Streblacantha circumtexta (Jørgensen, 1900). Paralectotype 1, PMO224.464/1, slide #65 (N36/2). Vestfjorden 13 January1899, 0–180 m. fig. 4.Streblacantha circumtexta (Jørgensen, 1900): a, b, paralectotype 2, PMO224.464/2, #slide 65 (N38/1). Vestfjorden 13 January 1899, 0–180 m. fig. 5.Streblacantha circumtexta (Jørgensen, 1900): a, b, paralectotype 3, PMO224.464/3, #slide 65 (O37/0). Vestfjorden 13 January 1899, 0–180 m. fig. 6.Stylodictya tenuispinaJørgensen, 1900: a, lectotype, PMO224.465, slide #54 (N37/0), Vesterålen 22 March 1899, 0–900 m; b, c, original drawings of Jørgensen (1900, pl. 10, fig. 39a and b) respectively. fig. 7.Stylodictya validispinaJørgensen, 1900: a, lectotype, PMO224.466, slide #54 (M37/0), Vesterålen 22 March 1899, 0–900 m; b, original drawing of Jørgensen (1900, pl. 10, fig. 40a). Note: where two or more images (a, b, –) are not otherwise described they represent different focal planes. Scale bar 100 μm.
Published: 01 January 2014
Explanation of Plate 3. fig. 1. Streblacantha circumtexta ( Jørgensen, 1900 ): a, b, lectotype, PMO224.463, slide #52 (O37/2), Tysfjord 28 March 1899, 0–700 m. fig. 2. Streblacantha circumtexta ( Jørgensen, 1900 ). Original drawing of Jørgensen (1900 , pl. 11, fig. 46a). fig. 3