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THE ORE DATABASE
Occurence 1848 - 006 Måløy
(Object Id: 2609)
(Last updated: 10.11.2023)

Location
County: Nordland Municipality: Steigen (1848)
Map 1:50000: Engelvær (2030-4) Map 1:250000: Bodø
Coordinate system: EU89-UTM Zone 33
East: 486470 m. North: 7521290 m.
Longitude: 14.6790350 Latitude: 67.8061850
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Resource
Resource Type: Ferroalloys (Cr,Ni,Co,V,Mo,W) Resource Subtype: Nickel
Element(s): Ni Cu Co
Importance
Raw material meaning: Little Importance (reg. 18.02.2015)

Resources and production
Activity: Test mining Reserves:
Operating method: Underground mining Historical production: ,1 thousand tons


Mineralization
Era: Paleozoic Period:
Genesis: Orthomagmatic formation Form: Lens
Main texture: Structureless Min. distribution: Disseminated (<20 % ore minerals)
Main grain size: Coarse grained (> 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
Sampler: P.M. Ihlen/L.P. Nilsson/...Stored: Løkken
Comment: Semi-massive pyrrhotite ore, with some dissemination of 1-3 mm prismatic amphibole aggregates
No. of registrated element analyses = 1
No. of registrated oxide analyses = 1
NO-MÅ-17-11A Bedrock
Sampler: P.M. Ihlen/L.P. Nilsson/...Stored: Løkken
Comment: Semi-massive sulphide min. Pl-rich gangue. Unalt. po-ptl assemb. in veins + dissem. in calcite marble
No. of registrated element analyses = 1
No. of registrated oxide analyses = 1
NO-MÅ-17-13B Dump
Sampler: P.M. Ihlen/L.P. Nilsson/...Stored: Løkken
Comment: Metagabbro, grain size 1-5 mm, with abundant pyrrhotite aggregates interstitial to amphibole-aggregates
No. of registrated element analyses = 1
No. of registrated oxide analyses = 1
NO-MÅ-17-9B Dump
Sampler: P.M. Ihlen/L.P. Nilsson/...Stored: Løkken
Comment: Amphibole pseudomorphs, 2-5 mm grain size, dark green, with interstitial net-veining of po-aggregates
No. of registrated element analyses = 1
No. of registrated oxide analyses = 1
NO-MÅ-17-9C Dump
Sampler: P.M. Ihlen/L.P. Nilsson/...Stored: Løkken
Comment: Amphibole pseudomorphs, 2-5 mm grain size, dark green, with interstitial net-veining of po-aggregates
No. of registrated element analyses = 1
No. of registrated oxide analyses = 1
NO0477.01 Bedrock
Sampler: Lindahl/Sørdal/...Stored: Løkken
No. of registrated element analyses = 1
NO0477.02 Bedrock
Sampler: Lindahl/Sørdal/...Stored: Løkken
No. of registrated element analyses = 1
NB! All analyse values are shown at the end of the printout.:


Analyse Results
from
Deposit Area 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


The fact sheet was created on 26.04.2024

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