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THE ORE DATABASE | |||||
Occurence 1824 - 011 Skravlåga | |||||
(Object Id: 2810) (Last updated: 28.04.2020) |
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Location |
County: | Nordland | Municipality: | Vefsn (1824) |
Map 1:50000: | Elsfjord (1927-3) | Map 1:250000: | Mo i Rana |
Coordinate system: | EU89-UTM Zone 33 |
East: | 430642 m. | North: | 7333633 m. |
Longitude: | 13.4647700 | Latitude: | 66.1154930 |
Show on map |
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Resource |
Resource Type: | Ferrous metals(Fe, Mn, Ti) | Resource Subtype: | Iron | |
Element(s): | Fe |
Importance |
Raw material meaning: | Little Importance (reg. 18.02.2015) |
Resources and production |
Activity: | Exploration | Reserves: | 6510 thousand tons | |
Operating method: | Historical production: |
Products |
Element/product | Crude ore grade or quality | Reg. date | |
Fe-mag. | 12 % | 06.01.1993 | |
Fe-total | 25 % | 06.01.1993 |
Operations |
From - To | Activity | Comments | |
1974 - 1975 | Geology | Company/Institution :Rana Gruber | |
1976 - 1976 | Geophysics | Company/Institution :Rana Gruber |
Mineralization |
Era: | Proterozoic | Period: | Neoproterozoic | |
Genesis: | Sedex | Form: | Layer | |
Main texture: | Banded | Min. distribution: | Semi-massive (20-50 % ore minerals) |
Main grain size: | Fine grained (< 1 mm) | Main alteration: |
Strike/Dip: | 35 / 80 | Direction: | 50 | |
Plunge: | 18 |
Stratigraphic classification of host rock |
Era: | Proterozoic | Period: | Neoproterozoic |
Province: | Caledonides | |
Geotec.unit: | Helgeland Nappe Complex | |
Tectonic complex: | Elsfjord unit | |
Igneous complex: |
Group: | Elsfjord-gruppen | Formation: |
Mineralogy |
Relationship | Mineral | Amount | |
Gangue mineral | Amphibole | Major mineral (>10%) | |
Gangue mineral | Quartz | Major mineral (>10%) | |
Gangue mineral | Epidote | Major mineral (>10%) | |
Gangue mineral | Carbonate | Subordinate mineral (1-10%) | |
Gangue mineral | Apatite | Accessory mineral (<1%) | |
Ore mineral | Magnetite | Major mineral (>10%) | |
Ore mineral | Hematite | Subordinate mineral (1-10%) |
Lithology: |
Relationship | Rock | Origin | |
Unknown | Karb.-aktinolittba. | Extrusive Original rock :Basalt |
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Metamorphic facies :Amphibolite | |||
Unknown | Amfibolitt | Extrusive Original rock :Basalt |
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Metamorphic facies :Amphibolite |
Structures |
Location: | Type: | Orientation(360 gr.): | Relation to min.: | |
Unknown | Primary layering | Strike/Dip :50 / 80 | Syn-mineralisation ;...Effect :None |
Information(s) in free text format |
Free text |
The rock sequence with iron formation at Skravlåga is well exposted along the river beds (WGS84 UTM 33N, 430400/7333850-430750/7333500). In the eastern part of the studied NW-SE trending river section occurs staurolite-bearing garnet-mica schist with consistent foliation and dip; 35°/85°. The schist is crosscut by tonalitic to granitic dykes/veins. Then follows an about 45 m thick unit of iron formation (susceptibility > 10,000 x 10-5 SI units). The IF is fine grained and commonly finely banded with both hematite and magnetite rich bands in few mm- to few cm-scale, and the matrix comprises mainly calcareous amphibole-epidote rock. Three samples were collected (Samples JS_FE 1704-06); from the hanging-wall, foot-wall and central part of the sequence, that represents the main locality for the deposit. No enrichment of Mn was observed. The IF is tectonostratgraphically underlain (up-river) by a nearly 300 m thick sequence of amphibole-mica-bearing calcareous schist. A few elongated lenses/clasts of dolomite is seen in this unit in the eastern 100 m of the sequence. Then occurs an about 50 m thick part with numerous dolomite clasts and the unit resembles diamictite. It is best exposed on the downside of a relatively recent constructed dam. A faint layering with layers in m-scale with various proportion of clasts exists. The clasts are generally strongly elongated and deformed. They are up to 1.5 m long and 10-20 cm thick and occur in a matrix of carbonate, amphibole and mica. An up to 30 cm thick lens of nearly massive, fine grained magnetite mineralisation in amphibole dominated matrix is observed within the diamictite as well as folded magnetite-rich bands in cm-scale (Sample JS_FE1708). Garnet-mica schist occurs in the western part of the section. |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | |||||
JS_FE1704 | Bedrock |
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JS_FE1705 | Bedrock |
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JS_FE1706 | Bedrock |
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NO0698.01 | Bedrock |
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NO0698.02 | Bedrock |
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NO0698.03 | Bedrock |
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NO0698.04 | Bedrock |
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NB! All analyse values are shown at the end of the printout.: |
Name of Sample point: Skravlåga dam |
(Object Id: 36440 11,00,01) |
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Location |
County: | Nordland | Municipality: | Vefsn (1824) |
Map 1:50000: | Elsfjord (1927-3) | Map 1:250000: | Mo i Rana |
Coordinate system: | EU89-UTM Zone 33 |
East: | 430516 m. | North: | 7333741 m. |
Longitude: | 13.4619420 | Latitude: | 66.1164360 |
Show on map |
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Resource |
Resource Type: | Ferrous metals(Fe, Mn, Ti) | Resource Subtype: | Iron | |
Element(s): | Fe |
Information(s) in free text format |
Free text |
Just east of the dam in Skravlåga occurs an about 50 m thick unit that resembles diamictite with numerous dolomite clasts. It is best exposed on the downside of the relatively recent constructed dam. A faint layering with layers in m-scale with various proportion of clasts exists. The clasts are generally strongly elongated and deformed. They are up to 1.5 m long and 10-20 cm thick and occur in a matrix of carbonate, amphibole and mica. An up to 30 cm thick lens of nearly massive, fine grained magnetite mineralisation in amphibole dominated matrix is observed within the diamictite as well as folded magnetite-rich bands in cm-scale (Sample JS_FE1708). |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | |||||
JS_FE1708 | Bedrock |
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NB! All analyse values are shown at the end of the printout.: |
Analyse Results |
from |
Deposit Area 1824 - 011 Skravlåga |
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# |
JS_FE1704 | Bedrock | 3 | 27 | 1 | 15 | 15 | 1.7 | |
JS_FE1705 | Bedrock | 2 | 24 | 1 | 10 | 11 | 1.5 | |
JS_FE1706 | Bedrock | 5 | 13 | 1 | 9 | 12 | -.5 | |
JS_FE1708 | Bedrock | 7 | 22 | 1 | 6 | 12 | .8 | |
NO0698.01 | Bedrock | 28 | 17 | -3 | 3 | 17 | -.3 | 6.0 |
NO0698.02 | Bedrock | 6 | 15 | -3 | 1 | 8 | -.3 | -2.0 |
NO0698.03 | Bedrock | 11 | 13 | 3 | 3 | 13 | -.3 | 5.0 |
NO0698.04 | Bedrock | 24 | 10 | 6 | 1 | 12 | -.3 | -2.0 |
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Sample No. | Pt# | Pd# | Rh# | As* | Cd* | Ba* | Mo* | Sn* | Sb* |
JS_FE1704 | 2 | 616 | 0.70 | 1 | |||||
JS_FE1705 | 1 | 374 | 0.50 | -1 | |||||
JS_FE1706 | 1 | 151 | 0.60 | -1 | |||||
JS_FE1708 | -1 | 207 | 0.80 | 1 | |||||
NO0698.01 | -3.0 | -3.0 | -5.0 | -2 | .5 | 17 | 3.00 | -2 | |
NO0698.02 | -3.0 | -3.0 | -5.0 | 3 | .4 | 14 | 1.00 | -2 | |
NO0698.03 | -3.0 | -3.0 | -5.0 | 4 | 1.6 | 8 | 1.00 | 4 | |
NO0698.04 | -3.0 | -3.0 | -5.0 | 2 | 2.1 | 17 | -1.00 | -2 |
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Sample No. | Bi* | Se* | Ga* | S% | V* | Cr* | Mn* | Fe% | Th* |
JS_FE1704 | -0.50 | 8.10 | 116 | 3.90 | |||||
JS_FE1705 | -0.50 | 6.20 | 82 | 2.50 | |||||
JS_FE1706 | -0.50 | 5.10 | 66 | 2.90 | |||||
JS_FE1708 | 3.30 | 7.80 | 92 | 4.30 | |||||
NO0698.01 | 13 | -.01 | 40 | 24 | 707 | 14.74 | 2.00 | ||
NO0698.02 | 3 | -.01 | 35 | 23 | 610 | 7.10 | 3.00 | ||
NO0698.03 | 23 | -.01 | 37 | 17 | 549 | 26.76 | 2.00 | ||
NO0698.04 | 29 | -.01 | 56 | 46 | 595 | 32.60 | 3.00 |
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Sample No. | U* | W* | Rb* | Sr* | Y* | Zr* | Nb* | Ta* | Cs* |
JS_FE1704 | 1.00 | -1 | 50.6 | 357.5 | 24.1 | 83 | 6.90 | 0.40 | 2.40 |
JS_FE1705 | 0.60 | 1 | 47.1 | 200.8 | 19.8 | 68 | 5.10 | 0.30 | 2.10 |
JS_FE1706 | 0.60 | 1 | 23.1 | 375.9 | 21.4 | 67 | 6.30 | 0.40 | 0.40 |
JS_FE1708 | 1.10 | -1 | 22.1 | 289.4 | 30.5 | 108 | 7.50 | 0.50 | 1.60 |
NO0698.01 | -5.00 | -2 | 72.0 | ||||||
NO0698.02 | -5.00 | -2 | 74.0 | ||||||
NO0698.03 | -5.00 | -2 | 12.0 | ||||||
NO0698.04 | -5.00 | -2 | 35.0 |
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Sample No. | La* | Ce* | Pr* | Nd* | Sm* | Eu* | Gd* | Tb* | Dy* |
JS_FE1704 | 29.90 | 67.00 | 7.78 | 32.70 | 6.07 | 1.31 | 5.74 | 0.86 | 5.03 |
JS_FE1705 | 15.70 | 32.90 | 4.01 | 16.40 | 3.11 | 0.71 | 3.12 | 0.49 | 3.25 |
JS_FE1706 | 16.80 | 34.20 | 4.01 | 15.30 | 3.06 | 0.79 | 3.34 | 0.54 | 3.39 |
JS_FE1708 | 22.60 | 45.40 | 5.62 | 23.30 | 4.22 | 0.94 | 4.39 | 0.71 | 4.40 |
NO0698.01 | 6.00 | ||||||||
NO0698.02 | 10.00 | ||||||||
NO0698.03 | 4.00 | ||||||||
NO0698.04 | 5.00 |
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Sample No. | Ho* | Er* | Tm* | Yb* | Lu* | B* | Be* | Hf* | |
JS_FE1704 | 0.93 | 2.80 | 0.39 | 2.41 | 0.37 | -1 | 2.10 | ||
JS_FE1705 | 0.65 | 2.12 | 0.29 | 2.02 | 0.32 | 1 | 1.40 | ||
JS_FE1706 | 0.72 | 2.20 | 0.33 | 2.07 | 0.35 | -1 | 1.70 | ||
JS_FE1708 | 0.96 | 2.95 | 0.43 | 2.85 | 0.45 | -1 | 2.80 | ||
NO0698.01 | -3 | ||||||||
NO0698.02 | -3 | ||||||||
NO0698.03 | -3 | ||||||||
NO0698.04 | -3 |
Oxide analyses |
( All values are in % ) |
Sample No. | Sample Type | SiO2 | Al2O3 | TiO2 | Fe2O3 | MnO | MgO | CaO |
JS_FE1704 | Bedrock | 18.20 | 4.53 | 0.42 | 68.40 | 0.59 | 2.35 | 3.42 |
JS_FE1705 | Bedrock | 33.00 | 4.47 | 0.31 | 51.20 | 0.15 | 3.90 | 4.64 |
JS_FE1706 | Bedrock | 39.10 | 4.47 | 0.38 | 37.30 | 0.39 | 3.09 | 9.76 |
JS_FE1708 | Bedrock | 42.90 | 6.47 | 0.60 | 35.80 | 0.01 | 3.21 | 6.58 |
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Sample No. | Na2O | K2O | P2O5 | Loss | Sum | ||||
JS_FE1704 | 0.86 | 1.24 | 0.92 | -1.33 | 100.00 | ||||
JS_FE1705 | 0.59 | 1.36 | 0.40 | -0.89 | 99.00 | ||||
JS_FE1706 | 0.61 | 0.61 | 0.52 | 2.67 | 99.00 | ||||
JS_FE1708 | 1.16 | 0.76 | 0.97 | 0.54 | 99.00 |
The fact sheet was created on 26.04.2024 |
Questions or comments regarding the fact sheet can be emailed to: ressursdatabaser@ngu.no |
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