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English version | ||||
| INDUSTRIMINERALDATABASEN | |||||
| Forekomstområde 1813 - 306 | |||||
| (Sist oppdatert 08.jul.2010) | |||||
Navn på deposit area : Rugåsen |
| (Objekt Id : 1813,306,00,00) |
| Lokalisering |
| Fylke : | Nordland (18) | Kommune : | Brønnøy (1813) |
| Kart 1:50000: | Velfjord (1825-4) | Kart 1:250000: | Mosjøen |
| Markeringspunkt: | Lengdegrad: | 12.5522260 | Breddegrad: | 65.4022930 |
| EU89-UTM Zone 33 | (Coordinates NOT confirmed) |
| X-koord: | 386332 m. | Y-koord: | 7255498 m. |
|
|
| Materialtype |
| Hovedtype: | Karbonatmineraler | Subtype: | Kalk |
| Betydning |
| Offentlig: | Not Assessed (reg. 18.02.2015) |
| Economical: | Ikke vurdert , (Confirmed 28.mar.2001 by Odd Øvereng) |
Products |
| Element/product | Crude ore grade or quality | |
| LIME | % |
Mineralization |
| Era: | Proterozoic | Period: | ||
| Dating: | Method: | |||
| Genesis: | Sedimentær/metamorf | Form: | ||
| Main texture: | Båndet | Min. distribution: |
| Main grain size: | Middelskornet (1-3 mm) |
| Strike/Dip: | Direction: | |||
| Plunge: |
| Stratigraphic classification of host rock |
| Era: | Proterozoic | Period: |
| Province: | Caledonides | |
| Geotec.unit: | Helgeland Nappe Complex | |
| Tectonic complex: | ||
| Igneous complex: |
| Group: | Formation: |
Bibliography: |
| From NGU's Reference Archive: |
| Myrland, Rolf , 1972 |
| Velfjord. Beskrivelse til det berggrunnsgeologiske gradteigskart I 18 - 1:100 000. |
| ;Norges geologiske undersøkelse;KARTBESKRIVELSE; TIDSSKRIFTARTIKKEL;NGU; Skrifter; No.274; 1;1-30 + ka pages |
| Abstract: | |
| The various lithologies are described. These comprise granitic basements rocks of supposed Pre-Cambrian age and Cambro-Silurian supracrustals and intrusives. The intrusives are mostly found within the Bindal and Velfjord massifs. These massifs are younger than the supracrustals, but their mutual age relationship is uncertain. Tectonically the rocks are sitated in "the high metamorphic nappe-complex" of central and western Helgeland. The supracrustal rocks have undergone at least three phases of Caledonian folding, the F2 phase producing the main regional structures. The rocks have mineral assemblages which place them in the almandine-amphibolite metamorphic facies. |
Fieldsamples |
| Sample No. | Sample type | Miscellanrous | |||||
| IL81 | Hand specimen |
|
| NB! All analyse values are shown at the end of the printout.: |
Analyse Results |
| from |
| Forekomstområde 1813 - 306 Rugåsen |
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* | As* |
| IL81 | Hand specimen | -2 | -1 | 3 | -4 | -2 | -10.0 | 18 |
| ------------------ |
| Sample No. | Cd* | Ba* | Mo* | Sn* | Sb* | Bi* | Se* | Ga* | Ge* |
| IL81 | -10.0 | 202 | -1.00 | -5 | -10 | 8 | 3.30 | -1.00 | -1.00 |
| ------------------ |
| Sample No. | V* | Cr* | Th* | U* | W* | Rb* | Sr* | Y* | Zr* |
| IL81 | -5 | -4 | -4.00 | -2.00 | -5 | 1.9 | 153.0 | -1.0 | -1 |
| ------------------ |
| Sample No. | Nb* | Ta* | Cs* | La* | Ce* | Nd* | Sm* | Yb* | Sc* |
| IL81 | -1.00 | -4.00 | -10.00 | -10.00 | -20.00 | -10.00 | -10.00 | -5.00 | -15.00 |
| ------------------ |
| Sample No. | Te* | Hf* | Hg* | Tl* | |||||
| IL81 | -10.00 | -5.00 | -4 | 9 |
Oxide analyses |
( All values are in % ) |
| Sample No. | Sample Type | SiO2 | Al2O3 | TiO2 | Fe2O3 | MnO | MgO | CaO |
| IL81 | Hand specimen | 0.48 | 0.11 | 0.01 | 0.12 | 0.02 | 0.62 | 55.44 |
| ------------------ |
| Sample No. | Na2O | K2O | P2O5 | Sum | |||||
| IL81 | -0.10 | 0.04 | -0.01 | 57.00 |
| Faktaarket ble generert 13.06.2026 |
| Spørsmål eller kommentarer vedrørende faktaarket kan mailes til: ressursdatabaser@ngu.no |
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