Norsk versjon | |||||
THE INDUSTRIAL MINERAL DATABASE | |||||
Occurence 1837 - 318 Ørnes | |||||
(Object Id: 15006) (Last updated: 11.10.2010) |
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Location |
County: | Nordland | Municipality: | Meløy (1837) |
Map 1:50000: | Meløy (1928-4) | Map 1:250000: | Mo i Rana |
Coordinate system: | EU89-UTM Zone 33 | (Coordinates NOT confirmed) |
East: | 442600 m. | North: | 7418500 m. |
Longitude: | 13.6899860 | Latitude: | 66.8790450 |
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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: |
Bucher-Nurminen, Kurt , 1988 |
Metamorphism of ultramafic rocks in the Central Scandinavian Caledonides |
;Norges geologiske undersøkelse;TIDSSKRIFTARTIKKEL;Special publication; No.3;86-95 pages |
Abstract: | |
Lenses and boudins of ultramafic rocks in the Central Scandinavian Caledonides (CSC) represent parts of dismembered ophiolite sequences and fragments of sub- continental upper mantle. The metaperidotites are isofacial with the metamorp- hic envelope, usually metasediments but in place also metagranitoids. Metamorphic assemblages in metaperidotites of the CSC, together with additional geological constraints, define a regional metamorphic gradient of prograde metamorphism which passes through the approximate PT-coordinates (in C and kbars): 400/4, 500/6, 600/8, 700/9. The sequence of prograde metamorphic assemblages is (with increasing temperature): antigorite+brucite, antigorite+ forsterite, forsterite+talc, forsterite+enstatite+chlorite, and forsterite+ enstatite+green spinel. The maximum temperature was not sufficient to replace calcic amphibole by calcic pyroxene. Pargasite overgrowth on earlier tremolite demonstrates the prograde nature of the metamorphism. Most of the ultramafic rocks probably represent progresively metamorphosed serpentinites (mantle-or crustal serpentinites?). The regional distribution of assemblages in the ultramafic rocks of the CSC defines a regular pattern which cross-cuts the nappe boundaries of the area. |
Gustavson, M.; Skauli, H. , 1990 |
Meløy. Berggrunnskart; Meløy; 19284; 1:50 000; sort/hvitt; |
;Norges geologiske undersøkelse;KART |
References not to be found in NGU's Reference Archive.: |
Sørensen, H. 1967: Metamorphic and metasomatic process in the formation of ultramafic rocks. In: Ultramafic and related rocks. Ed. P. J Wyllie. P 204-212. |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | |||
NGUAK96062 | Bedrock |
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NGUAK96063 | Bedrock |
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NB! All analyse values are shown at the end of the printout.: |
Analyse Results |
from |
Deposit Area 1837 - 318 Ørnes |
Oxide analyses |
( All values are in % ) |
Sample No. | Sample Type | SiO2 | Al2O3 | TiO2 | Fe2O3 | MnO | MgO | CaO |
NGUAK96062 | Bedrock | 42.50 | 0.84 | 0.00 | 10.70 | 0.15 | 38.20 | 0.19 |
NGUAK96063 | Bedrock | 46.80 | 0.74 | 0.00 | 7.30 | 0.15 | 22.90 | 13.58 |
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Sample No. | Na2O | K2O | P2O5 | Loss | Sum | ||||
NGUAK96062 | 0.03 | 0.28 | 0.00 | 6.74 | 100.00 | ||||
NGUAK96063 | 0.32 | 0.02 | 0.00 | 6.98 | 99.00 |
The fact sheet was created on 19.04.2024 |
Questions or comments regarding the fact sheet can be emailed to: ressursdatabaser@ngu.no |
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