English version | |||||
MALMDATABASEN | |||||
Forekomstområde 819 - 011 | |||||
(Sist oppdatert 20.mar.2024) |
Navn på forekomstområde : Søve |
(Objekt Id : 0819,011,00,00) |
Lokalisering |
Fylke : | Telemark (08) | Kommune : | Nome (0819) |
Kart 1:50000: | Nordagutu (1713-4) | Kart 1:250000: | Skien |
Markeringspunkt: | Lengdegrad: | 9.2849090 | Breddegrad: | 59.2819480 |
EU89-UTM Zone 32 |
X-koord: | 516234 m. | Y-koord: | 6571482 m. |
|
Materialtype |
Hovedtype: | Spesialmetaller (Nb,Ta,Be,Li,Sc,REE) | Subtype: | Niob | |
Element(er): | Nb Ta REE |
Produksjon |
Aktivitet: | Gruvedrift | Reserver: | ||
Prod. metode: | Dag- og underjordsdrift | Produksjon: | 1150 tusen tonn | |
Prod. status: | Nedlagt | Tippvolum: |
Betydning |
Offentlig: | Ikke vurdert (reg. 22.05.2015) |
Økonomisk: | Kan være viktig , (Stadfestet 07.des.2001 av Jan Sverre Sandstad) |
Produkt |
Element/produkt | Gehalt/Kvalitet | |
NB | 2800 ppm |
Operasjoner |
Fra - Til | Aktivitet | Kommentar | |
1951 - 1965 | Regulær drift | Selskap/Institusjon:Norsk Bergverk AS |
Mineralisering |
Æra: | Paleozoikum | Periode: | Kambrium | |
Datering: | Metode: | |||
Genese: | Intrusivbreksje/diatrem | Form: | ||
Hovedtextur: | Strukturløs | Min. fordeling: | Disseminert |
Kornstørrelse: | Finkornet (<1 mm) | Hovedomvandling: | Kalifeltspatomvandling |
Strøk/Fall: | Retning: | |||
Feltstupning: |
Stratigrafisk klassifikasjon av vertsbergart |
Æra: | Periode: |
Provins: | ||
Geotek.enhet: | ||
Tektonisk complex: | ||
Intrusivt komplex: |
Gruppe: | Formasjon: |
Mineralogi |
Relasjon | Mineral | Mengde | |
Gangmineral | Kalkspat | Hovedmineral (>10%) | |
Gangmineral | Glimmer | Underordnet mineral (1-10%) | |
Gangmineral | Apatitt | Underordnet mineral (1-10%) | |
Malmmineral | Pyroklor | Hovedmineral (>10%) | |
Malmmineral | Synchysitt | Aksessorisk mineral (<1%) | |
Malmmineral | Bastnäsitt | Aksessorisk mineral (<1%) | |
Malmmineral | Monazitt | Aksessorisk mineral (<1%) | |
Malmmineral | Parisitt | Aksessorisk mineral (<1%) |
Opplysning(er) i fritekstformat |
Fri tekst |
Fen is an early Cambrian silicate-carbonatite composite complex, which has a diameter of 5 km. It consists of a number of different intrusive to subvolcanic lithologies, including calcio- and ferrocarbonatites and various alkaline silicate rocks. The ferrocarbonatites are rich in ankerite and dolomite and contain Nb-, REE- and Th-rich minerals. In the eastern part of the complex, a red-colored carbonate- and oxide-rich rock unit occurs that is termed "rødbergite" (red rock). The red color is caused by finely dispersed hematite. Locally, the hematite is concentrated in dykes and veins and 1 mill t. of hematite ore was exploited by the Fen iron mines between 1657 until 1929. The rødberg rocks are rich in thorium and REE and resources are estimated to contain 170 000 t with 0.2 % Th and about 1 % REE (LREE). The calciocarbonatites (søvites) contain calcite, pyrochlore, biotite, REE-F-carbonates and monazite and the state-owned company AS Norsk Bergverk produced 1.15 mill t. of Nb-ore between 1953-1965 in the Søve mines, which gave 4100 t of Nb2O5. The pyrochlore is mainly concentrated along the margin of the carbonatite, but also related to breccia zones crosscutting the central part of the intrusion. |
Litteraturfortegnelser: |
Fra NGU's Referansearkiv.: |
Bergstøl, Sveinung; Svinndal, Sverre , 1960 |
Description of mines and deposits. Søve Niobium Mine, Fen area. |
;Norges geologiske undersøkelse;EKSKURSJONSGUIDE; TIDSSKRIFTARTIKKEL;NGU; No.212m;16-26 sider |
Bergstøl, Sveinung; Svinndal, Sverre , 1960 |
The carbonite and per-alkaline rocks of the Fen area. Petrology. |
;Norges geologiske undersøkelse;TIDSSKRIFTARTIKKEL;NGU; No.208;99-105 sider |
Sæther, Egil , 1957 |
The alkaline rock province of the Fen area in southern Norway. |
;ARTIKKEL;Det Kongelige Norske Videnskabers Selskabs Skrifter; No.1;150 s. sider |
Abstrakt: | |
An account is given of the field relationships, petrography, and mode of formation of alkaline silicate and carbonate rocks in the Cambro-Silurian Fen area in Telemarken, southwestern Norway. The Fen complex lies in Archean gneiss and gneissose granite and consists of the following rocks: granitic breccia; fenite (syenite); vipetoite, melteigite, ijolite, urtite (mafic alkalic rocks); damtjernite (hypabyssal rock); soevite (calcite rock); rauhaugite (ankerite rock); roedbergite or red rock (clacite-ankerite-hematite rock); and some dike rocks. Chemical rock and mineral analyses and spectrochemical analyses of oxide and sulfide minerals are presented, and optical data are given for many minerals. Substance transfers are computed for various metasomatic rock transformations in the area. Petrofabric diagrams of carbonatites are presented and interpreted. Genesis of the rocks is ascribed to two magmas poor in silica and rich in alkali metals, calcium, and carbon dioxide. Two separate cycles are established, each of which involved eruption of a mafic magma with subsequent very extensive hydrothermal activity (alkali metasomatism and carbonatization). The Fen area is compared with Alnø in Sweden, its close counterpart. |
Lie, Anders; Østergaard, Claus , 2011 |
The Fen carbonatite complex, Ulefoss, South Norway. Results and conclusions from preliminary microscope and microprobe studies |
;21st NORTH;RAPPORT;35 sider |
Lie, Anders; Østergaard, Claus , 2011 |
The Fen carbonatite complex, Ulefoss, South Norway. Summary of historic work and data |
;21st NORTH;RAPPORT;47 sider |
Andersen, Tom , 1983 |
Iron ores in the Fen central complex, Telemark (S.Norway): Petrography, chemical evolution and conditions of equilibrium |
;Norsk geologisk forening;TIDSSKRIFTARTIKKEL;Norsk geologisk tidsskrift; No.63 (2/3);73-82 sider |
Abstrakt: | |
Hydrothermal iron ores from the Fen central complex may be classified according to their mineral assemblages as primary (magnetite +- pyrite +- anatase + calcite) or secondary (hematite +- goethite + calcite +- dolomite). Primary ores equilibrated between the hematite-magnetite and magnetite-pyrite-pyrrho- tite buffers, at temperatures below 600°C. Alteration to form the secondary parageneses took place above the hematite-magnetite buffer, probably at lower temperature. |
Feltprøver |
Prøvenr. | Prøvetype | Diverse | |||
95394 | Fastfjell |
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95395 | Fastfjell |
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95397 | Fastfjell |
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95398 | Fastfjell |
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95399 | Fastfjell |
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95400 | Fastfjell |
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95401 | Fastfjell |
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95402 | Fastfjell |
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95403 | Fastfjell |
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95404 | Fastfjell |
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NB! Alle analyseverdier er vist i slutten av utskriften.: |
Analyseresultater |
fra |
Forekomstområde 819 - 011 Søve |
Elementanalyser |
( *=parts pr. million, #=parts pr.billion, Negative verdier betyr under deteksjonsgrensen.) |
Prøvenr. | Prøvetype | Co* | Ni* | Ba* | Sn* | Ga* | V* | Cr* |
95394 | Fastfjell | 10 | 730 | 1 | 4.40 | 133 | 21 | |
95395 | Fastfjell | 11 | 17301 | 7 | 8.40 | 89 | 103 | |
95397 | Fastfjell | 29 | 53 | 212 | 5 | 11.80 | 151 | 123 |
95398 | Fastfjell | 16 | 2073 | 1 | 10.40 | 134 | 116 | |
95399 | Fastfjell | 14 | 581 | 2 | 1.80 | 121 | ||
95400 | Fastfjell | 4 | 62 | 0.50 | 11 | |||
95401 | Fastfjell | 8 | 916 | 0.60 | 83 | |||
95402 | Fastfjell | 7 | 6941 | 6.90 | 77 | |||
95403 | Fastfjell | 13 | 642 | 1.60 | 18 | 21 | ||
95404 | Fastfjell | 5 | 83 | 2 | 2.80 | 28 | 41 |
------------------ |
Prøvenr. | Th* | U* | W* | Rb* | Sr* | Y* | Zr* | Nb* | Ta* |
95394 | 17.80 | 1.30 | 3.0 | 3920.7 | 58.3 | 259 | 59.50 | 6.90 | |
95395 | 782.30 | 3.70 | 5 | 3.2 | 1885.1 | 116.8 | 116 | 706.30 | 12.40 |
95397 | 1080.10 | 22.90 | 12 | 1.0 | 304.0 | 366.5 | 177 | 840.80 | 3.70 |
95398 | 1470.60 | 3.40 | 11 | 0.5 | 140.2 | 263.6 | 175 | 667.80 | 0.40 |
95399 | 19.30 | 0.90 | 1.0 | 3789.7 | 69.3 | 74 | 46.00 | 4.60 | |
95400 | 63.70 | 0.80 | 1 | 0.3 | 3800.9 | 24.8 | 50 | 2735.90 | 10.70 |
95401 | 28.60 | 113.60 | 6.0 | 4523.4 | 66.3 | 17 | 328.60 | 81.30 | |
95402 | 67.00 | 104.80 | 1 | 27.8 | 2938.1 | 138.9 | 365 | 421.50 | 58.30 |
95403 | 98.20 | 18.70 | 1 | 1.3 | 5147.8 | 83.6 | 64 | 821.50 | 6.00 |
95404 | 106.80 | 5.70 | 1 | 0.5 | 430.8 | 46.1 | 13 | 302.90 | 3.10 |
------------------ |
Prøvenr. | Cs* | La* | Ce* | Pr* | Nd* | Sm* | Eu* | Gd* | Tb* |
95394 | 0.30 | 269.50 | 527.20 | 60.24 | 218.50 | 32.87 | 9.36 | 24.83 | 2.68 |
95395 | 0.80 | 1516.20 | 2906.30 | 338.52 | 1269.70 | 237.85 | 64.87 | 137.05 | 11.00 |
95397 | 432.40 | 1066.50 | 163.27 | 808.70 | 231.68 | 54.55 | 148.03 | 15.09 | |
95398 | 0.10 | 1897.60 | 6680.90 | 1111.09 | 5046.40 | 546.73 | 94.51 | 163.71 | 10.31 |
95399 | 262.60 | 544.40 | 67.23 | 256.60 | 40.83 | 11.77 | 31.02 | 3.41 | |
95400 | 137.80 | 313.40 | 38.75 | 140.50 | 21.92 | 5.92 | 14.93 | 1.50 | |
95401 | 0.20 | 228.80 | 500.00 | 61.95 | 239.00 | 38.52 | 11.10 | 28.68 | 3.27 |
95402 | 0.20 | 541.90 | 1163.50 | 145.48 | 537.10 | 82.08 | 22.62 | 59.80 | 6.87 |
95403 | 0.30 | 1066.70 | 1778.80 | 209.41 | 813.20 | 139.91 | 31.32 | 62.38 | 4.51 |
95404 | 3289.60 | 4894.60 | 448.13 | 1334.30 | 116.53 | 14.30 | 56.96 | 3.49 |
------------------ |
Prøvenr. | Dy* | Ho* | Er* | Tm* | Yb* | Lu* | Be* | Hf* | |
95394 | 12.82 | 1.93 | 4.89 | 0.61 | 3.70 | 0.50 | 1 | 2.00 | |
95395 | 40.77 | 4.15 | 9.04 | 1.41 | 9.63 | 1.23 | 2 | 3.10 | |
95397 | 70.77 | 11.10 | 27.45 | 3.90 | 23.59 | 3.27 | 24 | 9.40 | |
95398 | 44.92 | 5.62 | 15.73 | 2.22 | 13.43 | 1.79 | 9 | 2.30 | |
95399 | 15.96 | 2.35 | 5.44 | 0.65 | 3.59 | 0.46 | 0.50 | ||
95400 | 6.40 | 0.96 | 2.14 | 0.25 | 1.28 | 0.15 | 0.90 | ||
95401 | 16.29 | 2.23 | 5.30 | 0.66 | 4.25 | 0.47 | 0.50 | ||
95402 | 32.95 | 5.00 | 12.00 | 1.47 | 8.21 | 1.06 | 3.50 | ||
95403 | 18.87 | 2.20 | 5.72 | 0.88 | 5.89 | 0.81 | 0.90 | ||
95404 | 12.41 | 0.99 | 2.13 | 0.32 | 2.28 | 0.26 |
Oksydanalyser |
(Alle verdier er i %) |
Prøvenr. | Prøvetype | SiO2 | Al2O3 | TiO2 | Fe2O3 | MnO | MgO | Na2O |
95394 | Fastfjell | 2.08 | 0.32 | 0.18 | 6.30 | 0.22 | 2.80 | 0.13 |
95395 | Fastfjell | 5.02 | 1.67 | 0.71 | 16.49 | 1.83 | 10.36 | 0.11 |
95397 | Fastfjell | 18.35 | 4.01 | 0.54 | 15.16 | 0.34 | 2.60 | 0.05 |
95398 | Fastfjell | 2.05 | 0.71 | 0.07 | 90.39 | 0.54 | 0.54 | |
95399 | Fastfjell | 0.65 | 0.27 | 0.17 | 5.61 | 0.18 | 2.03 | 0.03 |
95400 | Fastfjell | 0.75 | 0.02 | 3.42 | 0.60 | 17.06 | 0.01 | |
95401 | Fastfjell | 1.39 | 0.52 | 0.25 | 4.10 | 0.23 | 2.96 | 0.03 |
95402 | Fastfjell | 9.73 | 2.47 | 0.56 | 5.58 | 0.35 | 6.09 | 0.08 |
95403 | Fastfjell | 0.98 | 0.38 | 0.02 | 8.40 | 0.73 | 7.49 | 0.03 |
95404 | Fastfjell | 1.47 | 0.58 | 0.01 | 1.98 | 0.32 | 0.84 |
------------------ |
Prøvenr. | K2O | P2O5 | Loss | Sum | |||||
95394 | 0.06 | 4.26 | 35.00 | 51.00 | |||||
95395 | 0.07 | 0.24 | 35.70 | 72.00 | |||||
95397 | 0.01 | 0.63 | 24.70 | 66.00 | |||||
95398 | 0.02 | 0.67 | 0.30 | 95.00 | |||||
95399 | 0.03 | 3.35 | 37.20 | 50.00 | |||||
95400 | 4.16 | 40.70 | 67.00 | ||||||
95401 | 0.20 | 3.67 | 37.80 | 51.00 | |||||
95402 | 1.52 | 15.70 | 19.80 | 62.00 | |||||
95403 | 0.04 | 11.26 | 27.60 | 57.00 | |||||
95404 | 0.35 | 40.90 | 46.00 |
Faktaarket ble generert 25.11.2024 |
Spørsmål eller kommentarer vedrørende faktaarket kan mailes til: ressursdatabaser@ngu.no |
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