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English version | ||||
| MALMDATABASEN | |||||
| Forekomstområde 1848 - 006 | |||||
| (Sist oppdatert 10.nov.2023) | |||||
Navn på deposit area : Måløy |
| (Objekt Id : 1848,006,00,00) |
| Lokalisering |
| Fylke : | Nordland (18) | Kommune : | Steigen (1848) |
| Kart 1:50000: | Engelvær (2030-4) | Kart 1:250000: | Bodø |
| Markeringspunkt: | Lengdegrad: | 14.6790350 | Breddegrad: | 67.8061850 |
| EU89-UTM Zone 33 | (Coordinates IS confirmed) |
| X-koord: | 486470 m. | Y-koord: | 7521290 m. |
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| Materialtype |
| Hovedtype: | Jernlegeringsmetaller (Cr,Ni,Co,V,Mo,W) | Subtype: | Nikkel | |
| Element(s): | Ni Cu Co |
| Production |
| Activity: | Prøvedrift | Reserves: | ||
| Prod. method: | Underjordsdrift | Production: | ,1 thousand tons | |
| Prod. status: | Volume of dump: |
| Betydning |
| Offentlig: | Little Importance (reg. 18.02.2015) |
| Economical: | Lite viktig , (Confirmed 18.feb.2005 by Havard Gautneb) |
Mineralization |
| Era: | Paleozoic | Period: | ||
| Dating: | Method: | |||
| Genesis: | Ortomagmatisk | Form: | Linse | |
| Main texture: | Strukturløs | Min. distribution: | Disseminert |
| Main grain size: | Grovkornet (>3 mm) | Main alteration: |
| Strike/Dip: | Direction: | |||
| Plunge: |
| Stratigraphic classification of host rock |
| Era: | Paleozoic | Period: |
| Province: | Caledonides | |
| Geotec.unit: | Rødingsfjell Nappe Complex | |
| Tectonic complex: | ||
| Igneous complex: |
| Group: | Formation: |
Bibliography: |
| From NGU's Reference Archive: |
| Ihlen, Peter M.; Nilsson, Lars Petter , 2018 |
| Evaluation of Ni-Cu occurrences in the Uppermost Allochton of the Scandinavian Caledonides of Nordland, I: Field relationships |
| ;Norges geologiske undersøkelse;RAPPORT;NGU-rapport; No.2017.037;103 pages |
| Abstract: | |
| The report gives a description of the geology and field relationships of Ni-Cu mineralisation in 7 ore fields that occur in the Uppermost Allochthon (UmA) of the Scandinavian Caledonides in Nordland where they occur associated with a variety of metamorphosed and/or metasomatically altered mafic-ultramafic rock units. The occurrences in Markafjell in Brønnøy commune, Esjeholmene in Lurøy commune and Utvikåsen in Bodø commune are associated with ultramafic rocks in dismembered ophiolites whereas the ore-bearing ultramafic intrusion at Tverrbrennfjellet in Bodø commune comprises pyroxenites that have become “gabbroic” by mingling with a tonalitic magma. Mineralisation hosted by gabbroic intrusions are comprised by the Høgsetdalen showing in Gildeskål commune and the Lilleålegden deposit in Beiarn commune, as well as the Måløy deposit in Steigen commune. The latter two deposits have been the sites of small-scale mining in the past due to high-grade ores exceeding 1 wt. % (locally massive pentlandite with ca. 33 wt. % Ni). The Steinåga mineralisation in Beiarn commune comprising low-base metal pyrrhotite ore (< 0.1 wt % Ni or Cu) is hosted by ultramafic amphibolites possibly representing meta-volcanites. |
Fieldsamples |
| Sample No. | Sample type | Miscellanrous | |||||
| NO-MÅ-17-10C | Dump |
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| NO-MÅ-17-11A | Bedrock |
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| NO-MÅ-17-13B | Dump |
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| NO-MÅ-17-9B | Dump |
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| NO-MÅ-17-9C | Dump |
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| NO0477.01 | Bedrock |
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| NO0477.02 | Bedrock |
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| NB! All analyse values are shown at the end of the printout.: |
Analyse Results |
| from |
| Forekomstområde 1848 - 006 Måløy |
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* | Au# |
| NO-MÅ-17-10C | Dump | 981 | 120 | -5 | 401 | 22200 | ||
| NO-MÅ-17-11A | Bedrock | 1430 | 26 | -5 | 862 | 40400 | ||
| NO-MÅ-17-13B | Dump | 2480 | 167 | -5 | 295 | 14200 | ||
| NO-MÅ-17-9B | Dump | 1300 | 148 | -5 | 369 | 17600 | ||
| NO-MÅ-17-9C | Dump | 1510 | 144 | -5 | 291 | 15200 | ||
| NO0477.01 | Bedrock | 36758 | 132 | 6 | 453 | 23148 | 4.4 | 60.0 |
| NO0477.02 | Bedrock | 7198 | 74 | -3 | 350 | 19267 | .8 | 7.0 |
| ------------------ |
| Sample No. | Pt# | Pd# | Rh# | As* | Cd* | Ba* | Mo* | Sb* | Bi* |
| NO-MÅ-17-10C | -10 | 26 | |||||||
| NO-MÅ-17-11A | 14 | -10 | |||||||
| NO-MÅ-17-13B | 16 | 66 | |||||||
| NO-MÅ-17-9B | -10 | -10 | |||||||
| NO-MÅ-17-9C | 12 | 35 | |||||||
| NO0477.01 | 95.0 | 184.0 | -5.0 | 14 | 3.9 | 14 | 2.00 | 7 | -2 |
| NO0477.02 | 235.0 | 72.0 | -5.0 | 10 | 1.9 | 42 | 6.00 | 2 | -2 |
| ------------------ |
| Sample No. | S% | V* | Cr* | Mn* | Fe% | Th* | U* | W* | Sr* |
| NO-MÅ-17-10C | 15.50 | 117 | 352 | 20.80 | |||||
| NO-MÅ-17-11A | 32.80 | -5 | 106 | 22.70 | |||||
| NO-MÅ-17-13B | 10.30 | 101 | 295 | 19.60 | |||||
| NO-MÅ-17-9B | 13.50 | 98 | 441 | 20.10 | |||||
| NO-MÅ-17-9C | 11.20 | 103 | 436 | 19.30 | |||||
| NO0477.01 | 10.02 | 46 | 130 | 304 | 18.03 | 2.00 | -5.00 | -2 | 10.0 |
| NO0477.02 | 8.75 | 47 | 111 | 338 | 15.79 | 2.00 | -5.00 | -2 | 6.0 |
| ------------------ |
| Sample No. | Y* | Zr* | Nb* | La* | B* | Mg* | |||
| NO-MÅ-17-10C | 9.0 | 34 | -5.00 | 2 | |||||
| NO-MÅ-17-11A | 4.0 | 6 | -5.00 | 0 | |||||
| NO-MÅ-17-13B | 15.0 | 45 | 5.00 | 3 | |||||
| NO-MÅ-17-9B | 12.0 | 45 | -5.00 | 2 | |||||
| NO-MÅ-17-9C | 14.0 | 46 | 5.00 | 3 | |||||
| NO0477.01 | 2.00 | -3 | |||||||
| NO0477.02 | 3.00 | -3 |
Oxide analyses |
( All values are in % ) |
| Sample No. | Sample Type | SiO2 | Al2O3 | TiO2 | Fe2O3 | MnO | MgO | CaO |
| NO-MÅ-17-10C | Dump | 12.70 | 7.40 | 0.50 | 29.70 | 0.04 | 3.54 | 3.58 |
| NO-MÅ-17-11A | Bedrock | -0.50 | 0.30 | 0.03 | 32.40 | 0.02 | 0.25 | 1.33 |
| NO-MÅ-17-13B | Dump | 24.40 | 9.10 | 0.72 | 28.00 | 0.14 | 4.45 | 5.78 |
| NO-MÅ-17-9B | Dump | 17.70 | 7.30 | 0.60 | 28.70 | 0.07 | 3.98 | 4.75 |
| NO-MÅ-17-9C | Dump | 21.00 | 8.10 | 0.68 | 27.60 | 0.09 | 4.10 | 5.20 |
| ------------------ |
| Sample No. | Na2O | K2O | P2O5 | Loss | Sum | ||||
| NO-MÅ-17-10C | 1.02 | 0.47 | 0.06 | 20.00 | 79.00 | ||||
| NO-MÅ-17-11A | -0.10 | 0.03 | -0.01 | 44.60 | 78.00 | ||||
| NO-MÅ-17-13B | 1.16 | 0.32 | 0.08 | 11.90 | 86.00 | ||||
| NO-MÅ-17-9B | 1.01 | 0.29 | 0.11 | 16.90 | 81.00 | ||||
| NO-MÅ-17-9C | 1.13 | 0.28 | 0.11 | 15.00 | 83.00 |
| Faktaarket ble generert 13.06.2026 |
| Spørsmål eller kommentarer vedrørende faktaarket kan mailes til: ressursdatabaser@ngu.no |
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