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THE INDUSTRIAL MINERAL DATABASE | |||||
Occurence 1826 - 313 Krutvassrøddiken | |||||
(Object Id: 14992) (Last updated: 11.10.2010) |
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Location |
County: | Nordland | Municipality: | Aarborte (1826) |
Map 1:50000: | Trofors (1926-3) | Map 1:250000: | Mosjøen |
Coordinate system: | EU89-UTM Zone 33 |
East: | 468000 m. | North: | 7284999 m. |
Longitude: | 14.3035090 | Latitude: | 65.6852040 |
Show on map |
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Resource |
Resource Type: | Olivine | Resource Subtype: | Ultramafic (unspec.) |
Importance |
Raw material meaning: | Not Assessed (reg. 18.02.2015) |
Mineralization |
Genesis: | Form: | |||
Main texture: | Min. distribution: |
Main grain size: |
Strike/Dip: | Direction: | |||
Plunge: |
Stratigraphic classification of host rock |
Era: | Period: |
Province: | ||
Geotec.unit: | ||
Tectonic complex: | ||
Igneous complex: |
Group: | Formation: |
Bibliography: |
From NGU's Reference Archive: |
Stølen, Lars Kr. , 1985 |
Et geologisk studium av solitære ultramafiske bergarter og omkringliggende metasedimenter og metavulkanitter tilhørende Kølidekkene i Krutådalsområdet, Hattfjelldal, Nordland. |
;UiO Geologisk fellesråd;AVHANDLING |
Stigh, Jimmy , 1979 |
Ultramafites and detrial serpentinites in the central and southern parts of the Caledonian Allochthon in Scandinavia. |
;Chalmers Tekniska Högskola. Geologiska Institutionen;AVHANDLING;Publikation; No.A 27;222 s. pages |
Abstract: | |
Ultramafic rocks and detrial serpentinites in the central and southern part of the allochthon in Scandinavia have been investigated. The ultramafic bodies consist mainly of peridotites and olivinites, which are more or less serpentinised. Dunites, serpentinites, soapstones, sagvandites, harzburgites, and cortlandites also occur. These ultramafites appear as parts of layered intrusions and as isolated tectonic lenses. The latter are focussed in the present paper; they compose the great majority (>90 %) of the ultramafic rocks in the Scandinavian Caledonides. This category of rocks is referred to here as solitary, primitive ultramafites; being entirely composed of ultramafic material of mantle-like composition. (...) |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | |||
NGUAK96017 | Bedrock |
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NGUAK96018 | Bedrock |
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NGUAK96019 | Bedrock |
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NGUAK96020 | Bedrock |
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NGUAK96022 | Bedrock |
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NGUAK96023 | Bedrock |
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NGUAK96024 | Bedrock |
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NGUAK96025 | Bedrock |
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NGUAK96026 | Bedrock |
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NB! All analyse values are shown at the end of the printout.: |
Analyse Results |
from |
Deposit Area 1826 - 313 Krutvassrøddiken |
Oxide analyses |
( All values are in % ) |
Sample No. | Sample Type | SiO2 | Al2O3 | TiO2 | Fe2O3 | MnO | MgO | CaO |
NGUAK96017 | Bedrock | 39.20 | 0.48 | 0.00 | 10.00 | 0.09 | 40.20 | 0.06 |
NGUAK96018 | Bedrock | 40.70 | 0.38 | 0.00 | 7.50 | 0.11 | 44.60 | 0.04 |
NGUAK96019 | Bedrock | 40.60 | 0.37 | 0.00 | 7.00 | 0.08 | 44.70 | 0.04 |
NGUAK96020 | Bedrock | 39.30 | 0.33 | 0.00 | 9.00 | 0.14 | 47.30 | 0.05 |
NGUAK96022 | Bedrock | 40.70 | 0.41 | 0.00 | 8.40 | 0.11 | 44.90 | 0.14 |
NGUAK96023 | Bedrock | 39.90 | 0.19 | 0.00 | 9.60 | 0.15 | 48.50 | 0.06 |
NGUAK96024 | Bedrock | 40.50 | 0.30 | 0.00 | 8.60 | 0.12 | 44.70 | 0.20 |
NGUAK96025 | Bedrock | 40.20 | 0.28 | 0.00 | 8.20 | 0.11 | 44.10 | 0.14 |
NGUAK96026 | Bedrock | 40.80 | 0.29 | 0.00 | 8.30 | 0.12 | 44.00 | 0.22 |
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Sample No. | Na2O | K2O | P2O5 | Loss | Sum | ||||
NGUAK96017 | 0.00 | 0.00 | 0.00 | 9.41 | 99.00 | ||||
NGUAK96018 | 0.00 | 0.00 | 0.00 | 6.58 | 100.00 | ||||
NGUAK96019 | 0.03 | 0.00 | 0.00 | 6.70 | 100.00 | ||||
NGUAK96020 | 0.00 | 0.00 | 0.00 | 2.99 | 99.00 | ||||
NGUAK96022 | 0.00 | 0.00 | 0.00 | 5.29 | 100.00 | ||||
NGUAK96023 | 0.01 | 0.00 | 0.00 | 1.49 | 100.00 | ||||
NGUAK96024 | 0.00 | 0.00 | 0.00 | 5.48 | 100.00 | ||||
NGUAK96025 | 0.02 | 0.00 | 0.00 | 6.70 | 100.00 | ||||
NGUAK96026 | 0.00 | 0.00 | 0.00 | 6.06 | 100.00 |
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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