|
English version | ||||
| MALMDATABASEN | |||||
| Forekomstområde 1111 - 008 | |||||
| (Sist oppdatert 05.des.2025) | |||||
Navn på deposit area : Storgangen |
| (Objekt Id : 1111,008,00,00) |
| Lokalisering |
| Fylke : | Rogaland (11) | Kommune : | Sokndal (1111) |
| Kart 1:50000: | Sokndal (1311-4) | Kart 1:250000: | Mandal |
| Markeringspunkt: | Lengdegrad: | 6.3428180 | Breddegrad: | 58.3621470 |
| EU89-UTM Zone 32 | (Coordinates IS confirmed) |
| X-koord: | 344550 m. | Y-koord: | 6472100 m. |
|
|
| Materialtype |
| Hovedtype: | Jernmetaller (Fe, Mn, Ti) | Subtype: | Jern-titan | |
| Element(s): | Fe-Ti |
| Production |
| Activity: | Gruvedrift | Reserves: | 60000 thousand tons | |
| Prod. method: | Dag- og underjordsdrift | Production: | 10000 thousand tons | |
| Prod. status: | Nedlagt | Volume of dump: | 15000000 m3 | |
| Resource estimat. standard: | Ikke standardisert |
| Betydning |
| Offentlig: | International Importance (reg. 18.05.2015) |
| Economical: | Meget viktig , (Confirmed 18.mai.2015 by Henrik Schiellerup) |
Products |
| Element/product | Crude ore grade or quality | |
| TI | 11 % | |
| TIO2 | 18 % |
Operations |
| From - To | Activity | Comments | |
| 1902 - 1964 | Regular production | Company/Institution :Titania A/S | |
| Storgangen was mined by Titania A/S from 1902 to 1964. The mine produced a total of more than 10 Mt. of ore containing 18-19% TiO2, accounting for 11-13% of the world production of TiO2 during that periode (Krause m. fl. 1985). |
Mineralization |
| Era: | Proterozoic | Period: | Neoproterozoic | |
| Dating: | Method: | |||
| Genesis: | Ortomagmatisk | Form: | ||
| Main texture: | Båndet | Min. distribution: | Semi-massiv |
| Main grain size: | Middelskornet (1-3 mm) | Main alteration: |
| Strike/Dip: | Direction: | |||
| Plunge: |
| Ti-deposit type(s) |
| Main type: | Magmatic | Ilm/Mt-ratio: | ||
| Sub type: | Mt +/- Ilm +/- Ap in mafic intrusion | %TiO(Ore): | ||
| Titanium province: | Rogaland anorthosite province | %P2O5(Ore): | ||
| Host rock: | Norite | %MgO(Ilm): | ||
| Main Ti mineral: | Ilmenite | %V2O3(Mt): | ||
| ppm U (Rutile): |
| Stratigraphic classification of host rock |
| Era: | Proterozoic | Period: | Neoproterozoic |
| Province: | South Norwegian Basement Province | |
| Geotec.unit: | ||
| Tectonic complex: | ||
| Igneous complex: | Egersund Anorthosite Complex |
| Group: | Formation: |
Mineralogy |
| Relationship | Mineral | Amount | |
| Gangue mineral | Pyroxene | Major mineral (>10%) | |
| Gangue mineral | Plagioclase | Major mineral (>10%) | |
| Gangue mineral | Biotite | Subordinate mineral (1-10%) | |
| Ore mineral | Ilmenite | Major mineral (>10%) | |
| Ore mineral | Titanomagnetite | Major mineral (>10%) | |
| Ore mineral | Pyrrhotite | Subordinate mineral (1-10%) | |
| Ore mineral | Pyrite | Subordinate mineral (1-10%) | |
| Ore mineral | Chalcopyrite | Accessory mineral (<1%) | |
| Ore mineral | Pentlandite | Accessory mineral (<1%) |
Lithology: |
| Relationship | Rock | Origin | |
| Host rock | Magnetitt-ilmenitee-rik noritt | Intrusive Original rock :Norite |
|
| 949 (-7\+7) mill. years;..Method:U/Pb | |||
| Wall rock | Anortositt | Intrusive Original rock :Anorthosite |
Opplysning(er) i fritekstformat |
| Fri tekst |
| Storgangen er en 4 km lang og opp til 50 m mektig ØNØ-VSV'lig gangformet norittisk malmkropp i Åna-Sira anorthosittmassivet. Forekomsten er tolket å ha intrudert og størknet før den siste deformasjonen av anortositten (jfr. beskrivelse i Duchesne 2001) Malmkroppen er gjennomgående konkordant lagdelt i cm til m skala. Lagdelingen faller mot NNV med en vinkel varierende mellom 40 og 60 grader. De viktigste mineraler er plagioklas, Ca-fattig og Ca-rik pyroksen, apatitt, titanomagnetitt, ilmenitt, Cr-holdig spinell, diverse sulfidmineraler og baddeleitt. Forekomsten er generelt rik på oksyder over det hele, dog rikest i den nedre halvdel av stratigrafien. Aller nederst er ilmenitten en hemo-ilmenitt (Hem13) sammen med magnetitt og pleonaste spinell. MgO-innholdet i ilmenitt varierer fra 3-3.5% MgO nederst i stratigrafien til ca. 2% MgO mot toppen. Storgangen ble drevet av Titania fra 1916 til 1964. Det ble tilsammen produsert over 10 millioner tonn malm med i gjennomsnitt 18-19% TiO2. Dette tilsvarer 11-13% av verdensproduksjonen av ilmenitt i den samme perioden (Krause m. fl. 1985). |
Bibliography: |
| From NGU's Reference Archive: |
| Paludan, Johanne , 1995 |
| Structural evolution of the Bjerkreim-Sokndal layered intrusion, SW Norway: micro to macro scale studies. |
| ;AVHANDLING |
| Paludan, Johanne; Hansen, Ulla B.; Olesen, Niels Ø. , 1994 |
| Structural evolution of the Precambrian Bjerkreim-Sokndal intrusion, south Norway |
| ;Norsk geologisk forening;TIDSSKRIFTARTIKKEL;Norsk geologisk tidsskrift; No.74 (4);185-198 pages |
| Abstract: | |
| The structures of the northwestern part of the Precambrian Bjerkreim-Sokndal intrusion are studied from micro- to macro-scale. Meso-scale structures are dominated by (1) modal layering of igneous origin (Sg) and (2) prominent linear and planar fabrics (L1/S1), defined by the shape-preferred orientation of mineral aggregates. In most places So and S, are parallel, and together they define an isoclinal syncline with a southeastwards plunging fold axis. The linear fabric (L1) is subparallel to the fold axis in the hinge zone and converges towards this zone in the limbs. The intensity and type of fabric vary across the fold. In the hinge zone the L-fabric is dominant, whereas the rocks in the limbs display a combined S- and L-fabric. The intensity of the fabric is closely tied with microstructural indications of plastic deformation, such as lattice bending and kinking, polygonization and recrystallization. All of this points to one major phase of solid state deformation. Estimates of the strain state are based on regional variations in the shape of olivine grains and aggregates from two igneous units.Extensions of up to 100% are observed in the hinge zone, and flattening around 40% is observed in the south- ern limb. Rheological considerations suggest that these are minimum values. In our interpretation, the deformation was the result of passive subsidence of the intrusive rocks, induced by gravitational instabilities in the area (inverse diapirism) A convergent flow pattern led to the formation of L-tec- tonites in the hinge zone and an additional shear component along the limb led to the formation of L/S-tectonites. A series of monzonorite dykes (the Lomland dykes) and a number of minor shear zones all post-date the major deformation. The dykes and shear zones may be coeval. |
| References not to be found in NGU's Reference Archive.: |
| Bolle, O., Diot, H. & Duchesne, J.C. 2000: Magnetic fabric and deformation in charnockitic igneous rocks of the Bjerkreim-Sokndal layered intrusion (Rogaland, Southwest Norway). J. Struct. Geol. 22, 647-667. |
| Duchesne, J.-C. 2001: The Rogaland Intrusive Massifs - an excursion guide. NGU Report 2001.029, 139 p. (ISBN 82-7385-198-2). |
Fieldsamples |
| Sample No. | Sample type | Miscellanrous | |||||
| 160861 | Bedrock |
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| 160862 | Bedrock |
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| 160863 | Bedrock |
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| 160864 | Bedrock |
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| 160865 | Bedrock |
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| 160866 | Bedrock |
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| 160867 | Bedrock |
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| 160868 | Bedrock |
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| 160869 | Bedrock |
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| 160870 | Bedrock |
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| 160871 | Bedrock |
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| 160872 | Bedrock |
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| 160873 | Bedrock |
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| 160874 | Bedrock |
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| NB! All analyse values are shown at the end of the printout.: |
Navn på locality : Aursland skjerp |
| (Objekt Id : 1111,008,01,00) |
| Lokalisering |
| Fylke : | Rogaland (11) | Kommune : | Sokndal (1111) |
| Kart 1:50000: | Sokndal (1311-4) | Kart 1:250000: | Mandal |
| Markeringspunkt: | Lengdegrad: | 6.3745360 | Breddegrad: | 58.3610040 |
| EU89-UTM Zone 32 | (Coordinates IS confirmed) |
| X-koord: | 346400 m. | Y-koord: | 6471899 m. |
|
|
| Materialtype |
| Hovedtype: | Jernmetaller (Fe, Mn, Ti) | Subtype: | Jern-titan | |
| Element(s): | Fe Ti P |
Navn på locality : Sidegangen |
| (Objekt Id : 1111,008,02,00) |
| Lokalisering |
| Fylke : | Rogaland (11) | Kommune : | Sokndal (1111) |
| Kart 1:50000: | Sokndal (1311-4) | Kart 1:250000: | Mandal |
| Markeringspunkt: | Lengdegrad: | 6.3384820 | Breddegrad: | 58.3629550 |
| EU89-UTM Zone 32 | (Coordinates IS confirmed) |
| X-koord: | 344299 m. | Y-koord: | 6472199 m. |
|
|
| Materialtype |
| Hovedtype: | Jernmetaller (Fe, Mn, Ti) | Subtype: | Jern-titan | |
| Element(s): | Fe Ti P |
Navn på locality : Sidegangen 2 |
| (Objekt Id : 1111,008,03,00) |
| Lokalisering |
| Fylke : | Rogaland (11) | Kommune : | Sokndal (1111) |
| Kart 1:50000: | Sokndal (1311-4) | Kart 1:250000: | Mandal |
| Markeringspunkt: | Lengdegrad: | 6.3452100 | Breddegrad: | 58.3644430 |
| EU89-UTM Zone 32 | (Coordinates IS confirmed) |
| X-koord: | 344699 m. | Y-koord: | 6472350 m. |
|
|
| Materialtype |
| Hovedtype: | Jernmetaller (Fe, Mn, Ti) | Subtype: | Jern-titan | |
| Element(s): | Fe Ti P |
Navn på locality : Sidegangen 2 forts. |
| (Objekt Id : 1111,008,04,00) |
| Lokalisering |
| Fylke : | Rogaland (11) | Kommune : | Sokndal (1111) |
| Kart 1:50000: | Sokndal (1311-4) | Kart 1:250000: | Mandal |
| Markeringspunkt: | Lengdegrad: | 6.3473330 | Breddegrad: | 58.3703280 |
| EU89-UTM Zone 32 | (Coordinates IS confirmed) |
| X-koord: | 344849 m. | Y-koord: | 6473000 m. |
|
|
| Materialtype |
| Hovedtype: | Jernmetaller (Fe, Mn, Ti) | Subtype: | Jern-titan | |
| Element(s): | Fe Ti P |
Navn på locality : Sidegangen 3 |
| (Objekt Id : 1111,008,05,00) |
| Lokalisering |
| Fylke : | Rogaland (11) | Kommune : | Sokndal (1111) |
| Kart 1:50000: | Sokndal (1311-4) | Kart 1:250000: | Mandal |
| Markeringspunkt: | Lengdegrad: | 6.3537800 | Breddegrad: | 58.3641710 |
| EU89-UTM Zone 32 | (Coordinates IS confirmed) |
| X-koord: | 345199 m. | Y-koord: | 6472299 m. |
|
|
| Materialtype |
| Hovedtype: | Jernmetaller (Fe, Mn, Ti) | Subtype: | Jern-titan | |
| Element(s): | Fe Ti P |
Navn på sample point : test |
| (Objekt Id : 1111,008,05,01) |
| Lokalisering |
| Fylke : | Rogaland (11) | Kommune : | Sokndal (1111) |
| Kart 1:50000: | Sokndal (1311-4) | Kart 1:250000: | Mandal |
| Markeringspunkt: | (Unavailable) |
|
|
| Materialtype |
| Hovedtype: | Jernmetaller (Fe, Mn, Ti) | Subtype: | Jern-titan | |
| Element(s): | Fe Ti |
Analyse Results |
| from |
| Forekomstområde 1111 - 008 Storgangen |
Element analyses |
( *=parts pr. million, #=parts pr.billion, Negative values means below detection limit value.) |
| Sample No. | Sample Type | Cu* | Zn* | Pb* | Co* | Ni* | Ag* | As* |
| 160861 | Bedrock | 215 | 188 | 11 | 133 | 339 | .5 | 5 |
| 160862 | Bedrock | 350 | 254 | 10 | 180 | 505 | .5 | 5 |
| 160863 | Bedrock | 166 | 207 | 13 | 142 | 337 | .5 | 5 |
| 160864 | Bedrock | 145 | 176 | 12 | 124 | 296 | .5 | 5 |
| 160865 | Bedrock | 163 | 154 | 19 | 146 | 321 | .5 | 5 |
| 160866 | Bedrock | 116 | 148 | 10 | 111 | 256 | .5 | 5 |
| 160867 | Bedrock | 27 | 57 | 1 | 29 | 63 | .5 | 5 |
| 160868 | Bedrock | 148 | 211 | 11 | 165 | 293 | .5 | 5 |
| 160869 | Bedrock | 101 | 190 | 9 | 126 | 207 | .5 | 6 |
| 160870 | Bedrock | 368 | 232 | 14 | 204 | 519 | .5 | 5 |
| 160871 | Bedrock | 162 | 172 | 8 | 127 | 344 | .5 | 5 |
| 160872 | Bedrock | 299 | 242 | 13 | 187 | 447 | .5 | 5 |
| 160873 | Bedrock | 249 | 193 | 12 | 161 | 343 | .5 | 5 |
| 160874 | Bedrock | 147 | 209 | 9 | 160 | 265 | .5 | 5 |
| ------------------ |
| Sample No. | Cd* | Ba* | Mo* | Sn* | Ga* | V* | Cr* | Th* | U* |
| 160861 | 1.3 | 68 | 1.00 | 1 | 18.60 | 994 | 136 | 0.05 | 0.02 |
| 160862 | 1.8 | 36 | 1.00 | 1 | 18.40 | 1215 | 141 | 0.05 | 0.02 |
| 160863 | 1.5 | 49 | 1.00 | 1 | 15.40 | 1000 | 150 | 0.05 | 0.02 |
| 160864 | 1.7 | 101 | 1.00 | 1 | 22.80 | 1275 | 194 | 0.05 | 0.02 |
| 160865 | 1.6 | 50 | 1.00 | 2 | 16.20 | 1375 | 193 | 0.05 | 0.02 |
| 160866 | 1.2 | 120 | 1.00 | 1 | 20.80 | 906 | 111 | 0.05 | 0.02 |
| 160867 | .5 | 310 | 1.00 | 1 | 25.60 | 221 | 23 | 0.10 | 0.06 |
| 160868 | 1.6 | 21 | 1.00 | 1 | 18.20 | 1120 | 85 | 0.05 | 0.02 |
| 160869 | 1.2 | 70 | 1.00 | 1 | 15.70 | 769 | 50 | 0.05 | 0.02 |
| 160870 | 1.9 | 13 | 1.00 | 1 | 17.40 | 1265 | 86 | 0.05 | 0.02 |
| 160871 | 1.0 | 84 | 1.00 | 1 | 14.60 | 741 | 171 | 0.09 | 0.02 |
| 160872 | 1.7 | 8 | 1.00 | 1 | 15.90 | 1190 | 81 | 0.06 | 0.02 |
| 160873 | 1.6 | 47 | 1.00 | 1 | 15.70 | 995 | 81 | 0.09 | 0.02 |
| 160874 | 1.5 | 41 | 1.00 | 1 | 15.00 | 936 | 79 | 0.07 | 0.02 |
| ------------------ |
| Sample No. | W* | Rb* | Sr* | Y* | Zr* | Nb* | Ta* | Cs* | La* |
| 160861 | 1 | 0.8 | 179.0 | 2.7 | 116 | 14.50 | 1.10 | 0.01 | 0.80 |
| 160862 | 1 | 0.8 | 72.0 | 2.8 | 154 | 17.45 | 1.30 | 0.01 | 0.30 |
| 160863 | 1 | 0.7 | 121.0 | 2.6 | 121 | 14.95 | 1.10 | 0.01 | 0.90 |
| 160864 | 1 | 0.9 | 263.0 | 1.5 | 175 | 22.30 | 1.70 | 0.01 | 1.10 |
| 160865 | 1 | 0.3 | 123.5 | 1.4 | 214 | 29.20 | 2.10 | 0.01 | 0.50 |
| 160866 | 1 | 0.9 | 317.0 | 1.9 | 125 | 15.55 | 1.00 | 0.01 | 1.20 |
| 160867 | 1 | 3.2 | 744.0 | 3.9 | 45 | 4.09 | 0.20 | 0.01 | 4.60 |
| 160868 | 1 | 0.3 | 49.9 | 3.0 | 122 | 14.70 | 1.00 | 0.01 | 0.40 |
| 160869 | 1 | 0.6 | 182.0 | 3.2 | 94 | 10.55 | 0.40 | 0.01 | 0.70 |
| 160870 | 1 | 0.2 | 26.8 | 2.9 | 142 | 16.85 | 1.30 | 0.01 | 0.20 |
| 160871 | 1 | 0.9 | 218.0 | 6.6 | 128 | 17.15 | 1.20 | 0.03 | 1.70 |
| 160872 | 13 | 0.2 | 18.4 | 3.4 | 138 | 15.75 | 1.30 | 0.02 | 0.30 |
| 160873 | 4 | 0.6 | 115.5 | 3.5 | 137 | 15.15 | 1.20 | 0.02 | 1.30 |
| 160874 | 1 | 0.3 | 107.5 | 3.5 | 117 | 13.25 | 1.10 | 0.02 | 0.90 |
| ------------------ |
| Sample No. | Ce* | Pr* | Nd* | Sm* | Eu* | Gd* | Tb* | Dy* | Ho* |
| 160861 | 1.80 | 0.27 | 1.10 | 0.26 | 0.30 | 0.38 | 0.07 | 0.45 | 0.11 |
| 160862 | 1.20 | 0.21 | 0.80 | 0.30 | 0.17 | 0.29 | 0.06 | 0.47 | 0.11 |
| 160863 | 1.80 | 0.23 | 1.00 | 0.26 | 0.19 | 0.35 | 0.06 | 0.35 | 0.10 |
| 160864 | 2.20 | 0.30 | 1.10 | 0.29 | 0.39 | 0.24 | 0.03 | 0.29 | 0.07 |
| 160865 | 1.20 | 0.14 | 0.60 | 0.09 | 0.20 | 0.19 | 0.03 | 0.25 | 0.07 |
| 160866 | 2.20 | 0.25 | 0.90 | 0.18 | 0.48 | 0.30 | 0.06 | 0.34 | 0.08 |
| 160867 | 10.40 | 1.21 | 5.90 | 1.32 | 1.18 | 1.20 | 0.16 | 0.90 | 0.15 |
| 160868 | 0.90 | 0.12 | 0.70 | 0.19 | 0.10 | 0.29 | 0.06 | 0.48 | 0.13 |
| 160869 | 1.70 | 0.19 | 0.90 | 0.29 | 0.28 | 0.38 | 0.08 | 0.43 | 0.11 |
| 160870 | 0.80 | 0.10 | 0.50 | 0.19 | 0.10 | 0.31 | 0.07 | 0.47 | 0.11 |
| 160871 | 3.80 | 0.51 | 1.90 | 0.54 | 0.39 | 0.76 | 0.19 | 0.93 | 0.26 |
| 160872 | 0.70 | 0.12 | 0.20 | 0.14 | 0.04 | 0.23 | 0.07 | 0.34 | 0.13 |
| 160873 | 2.30 | 0.33 | 0.90 | 0.26 | 0.17 | 0.32 | 0.10 | 0.38 | 0.14 |
| 160874 | 1.60 | 0.24 | 0.60 | 0.16 | 0.15 | 0.36 | 0.09 | 0.34 | 0.14 |
| ------------------ |
| Sample No. | Er* | Tm* | Yb* | Lu* | Li* | Sc* | Hf* | Tl* | |
| 160861 | 0.32 | 0.06 | 0.45 | 0.07 | 10 | 30.00 | 3.43 | 10 | |
| 160862 | 0.35 | 0.07 | 0.46 | 0.07 | 10 | 35.00 | 4.08 | 10 | |
| 160863 | 0.25 | 0.05 | 0.43 | 0.06 | 10 | 33.00 | 3.33 | 10 | |
| 160864 | 0.24 | 0.04 | 0.28 | 0.07 | 10 | 30.00 | 4.82 | 10 | |
| 160865 | 0.17 | 0.04 | 0.27 | 0.06 | 10 | 40.00 | 6.32 | 20 | |
| 160866 | 0.22 | 0.05 | 0.33 | 0.06 | 10 | 27.00 | 3.71 | 10 | |
| 160867 | 0.40 | 0.05 | 0.31 | 0.04 | 10 | 7.00 | 1.20 | 10 | |
| 160868 | 0.39 | 0.07 | 0.45 | 0.07 | 10 | 35.00 | 3.42 | 10 | |
| 160869 | 0.34 | 0.06 | 0.51 | 0.07 | 10 | 28.00 | 2.49 | 10 | |
| 160870 | 0.33 | 0.06 | 0.44 | 0.07 | 10 | 36.00 | 3.79 | 20 | |
| 160871 | 0.77 | 0.13 | 0.78 | 0.12 | 10 | 32.00 | 3.89 | 10 | |
| 160872 | 0.44 | 0.08 | 0.50 | 0.09 | 10 | 36.00 | 3.52 | 10 | |
| 160873 | 0.44 | 0.08 | 0.48 | 0.08 | 10 | 32.00 | 3.59 | 10 | |
| 160874 | 0.40 | 0.08 | 0.49 | 0.10 | 10 | 32.00 | 3.22 | 10 |
Oxide analyses |
( All values are in % ) |
| Sample No. | Sample Type | SiO2 | Al2O3 | TiO2 | Fe2O3 | MnO | MgO | CaO |
| 160861 | Bedrock | 30.20 | 6.82 | 16.60 | 35.40 | 0.22 | 10.10 | 2.41 |
| 160862 | Bedrock | 22.90 | 3.79 | 20.10 | 43.30 | 0.24 | 9.64 | 1.36 |
| 160863 | Bedrock | 25.50 | 5.39 | 19.10 | 37.90 | 0.23 | 9.30 | 1.88 |
| 160864 | Bedrock | 20.70 | 8.88 | 23.20 | 40.40 | 0.18 | 4.48 | 2.76 |
| 160865 | Bedrock | 13.55 | 4.57 | 29.80 | 44.80 | 0.22 | 5.45 | 1.46 |
| 160866 | Bedrock | 31.20 | 10.20 | 17.05 | 30.80 | 0.18 | 6.98 | 3.54 |
| 160867 | Bedrock | 50.00 | 22.30 | 3.44 | 8.62 | 0.06 | 2.62 | 7.67 |
| 160868 | Bedrock | 27.20 | 3.19 | 17.40 | 40.90 | 0.27 | 12.55 | 1.24 |
| 160869 | Bedrock | 35.80 | 7.07 | 12.55 | 31.00 | 0.22 | 11.75 | 2.65 |
| 160870 | Bedrock | 21.60 | 2.47 | 19.30 | 45.00 | 0.28 | 10.65 | 0.99 |
| 160871 | Bedrock | 34.70 | 7.25 | 13.70 | 29.20 | 0.24 | 11.15 | 3.02 |
| 160872 | Bedrock | 24.50 | 2.21 | 18.35 | 42.50 | 0.29 | 12.30 | 1.03 |
| 160873 | Bedrock | 28.10 | 4.87 | 16.85 | 37.50 | 0.27 | 11.30 | 1.86 |
| 160874 | Bedrock | 31.40 | 4.72 | 14.60 | 35.00 | 0.27 | 12.60 | 1.88 |
| ------------------ |
| Sample No. | Na2O | K2O | P2O5 | Loss | Sum | ||||
| 160861 | 1.03 | 0.17 | 0.02 | -1.01 | 102.00 | ||||
| 160862 | 0.36 | 0.08 | 0.01 | -0.92 | 101.00 | ||||
| 160863 | 0.72 | 0.13 | 0.02 | -0.86 | 99.00 | ||||
| 160864 | 1.41 | 0.22 | 0.02 | -1.45 | 101.00 | ||||
| 160865 | 0.66 | 0.11 | 0.01 | -2.31 | 98.00 | ||||
| 160866 | 1.82 | 0.27 | 0.03 | -1.15 | 101.00 | ||||
| 160867 | 4.32 | 0.69 | 0.11 | 0.17 | 100.00 | ||||
| 160868 | 0.22 | 0.05 | 0.01 | -1.61 | 101.00 | ||||
| 160869 | 1.05 | 0.16 | 0.02 | -0.35 | 102.00 | ||||
| 160870 | 0.22 | 0.05 | -0.01 | -1.39 | 99.00 | ||||
| 160871 | 1.21 | 0.22 | 0.04 | -0.91 | 100.00 | ||||
| 160872 | 0.12 | 0.03 | 0.01 | -1.46 | 100.00 | ||||
| 160873 | 0.64 | 0.13 | 0.03 | -1.29 | 100.00 | ||||
| 160874 | 0.61 | 0.11 | -0.01 | -1.32 | 100.00 |
| Faktaarket ble generert 10.06.2026 |
| Spørsmål eller kommentarer vedrørende faktaarket kan mailes til: ressursdatabaser@ngu.no |
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