(Last updated: 07.11.2006)
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Norsk versjon | ||||
| THE ???? DATABASE | |||||
| Occurence 0 - 000 FEIL | |||||
| (Object Id: ) (Last updated: 07.11.2006) |
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| Location |
| County: | Municipality: | Mangler () |
| Map 1:50000: | Mo i Rana (1927-1) | Map 1:250000: | Mo i Rana |
| Coordinate system: | UTM-Zone 33 - EUREF89/WGS84 |
| East: | 458000 m. | North: | 7362900 m. |
| Longitude: | 14.0605930 | Latitude: | 66.3811680 |
| Show on map |
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| Resource |
| Resource Type: | Carbonates | Resource Subtype: | Limestone |
| Importance |
| Raw material meaning: | Not Assessed (reg. 07.12.2015) |
Products |
| Element/product | Crude ore grade or quality | Reg. date | |
| Agricultural lime | 05.12.2000 | ||
| Metallurgical use | 05.12.2000 |
Operations |
| From - To | Activity | Comments | |
| 1998 - 1998 | Geochemistry | Company/Institution :NGU | |
| 1998 - 1998 | Sampling | Company/Institution :NGU |
Mineralization |
| Era: | Paleozoic | Period: | ||
| Genesis: | Sedimentary/metamorphic | Form: | Layer | |
| Main texture: | Banded | Min. distribution: | Massive (>50 % ore minerals) |
| Main grain size: | Fine - medium grained (<1mm - 3 mm) |
| 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: |
Mineralogy |
| Mineral | Amount | |
| Calcite | Major mineral (>90%) | |
| Quartz | Subordinate mineral (1-10%) | |
| Feldspar | Subordinate mineral (1-10%) | |
| Mica | Subordinate mineral (1-10%) | |
| Pyrite | Accessory mineral (<1%) | |
| Apatite | Accessory mineral (<1%) | |
| Graphite | Accessory mineral (<1%) | |
| Dolomite | Accessory mineral (<1%) |
Structures |
| Location: | Type: | Orientation(360 gr.): | Relation to min.: | |
| Host rock | Foliation | Strike/Dip :20 / 40 |
Information(s) in free text format |
| Free text |
| I vegskjæringen ute på Kvitneset er det en veksllagning mellom grå båndet urein og hvit middelskornet kalkspatmarmor. Den hvite kalkspatmarmoren virket homogen og lite forurenset. Den har stedvis diffuse grå flammestrukturer. De grå flammestrukturene består i hovedsak av finfordelt grafitt. Foliasjonen i den grå ureine kalkspatmarmoren er N 20° Ø og fall 40° Ø. Prøve merket Ø98 - 30. Dagbok OØ1998. |
Bibliography: |
| From NGU's Reference Archive: |
| Zwaan, Klaas B. , 1970 |
| Prøvetaking Langvatn kalk-dolomittbånd. |
| ;Norges geologiske undersøkelse;FAGRAPPORT;Bergarkivet; No.BA 6495;5 pages |
| Abstract: | |
| Prøver av kalk-dolomittbåndene langs nordsiden av Langvatnet. Prøvebeskrivel- sen antyder små mektigheter (-10 m), sterke foldinger og vekslinger med vesentlig glimmerskifer. Beskrives dels som uren. I alt 14 analyser presenteres. |
Fieldsamples |
| Sample No. | Sample type | Miscellanrous | ||||
| NO0151.1 | Hand specimen |
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| NB! All analyse values are shown at the end of the printout.: |
| The fact sheet was created on 07.05.2024 |
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