(Last updated: 11.02.1997)
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Norsk versjon | ||||
| THE ORE DATABASE | |||||
| Occurence 4617 - 043 Sandvikfjell | |||||
| (Object Id: 4868) (Last updated: 11.02.1997) |
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| Location |
| County: | Vestland | Municipality: | Kvinnherad (4617) |
| Map 1:50000: | Varaldsøy (1215-2) | Map 1:250000: | Bergen |
| Coordinate system: | EU89-UTM Zone 32 |
| East: | 329879 m. | North: | 6668607 m. |
| Longitude: | 5.9382830 | Latitude: | 60.1190040 |
| Show on map |
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| Resource |
| Resource Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Resource Subtype: | Sulphides | |
| Element(s): | Kis |
| Importance |
| Raw material meaning: | Not Assessed (reg. 18.02.2015) |
| Resources and production |
| Activity: | Test mining | Reserves: | ||
| Operating method: | Open pit and underground mining | Historical production: |
Operations |
| From - To | Activity | Comments | |
| Test mining |
Mineralization |
| Era: | Paleozoic | Period: | Ordovician | |
| Genesis: | Volcex | Form: | Layer | |
| Main texture: | Banded | Min. distribution: | Semi-massive (20-50 % ore minerals) |
| Main grain size: | Medium grained (1-3 mm) | Main alteration: |
| Strike/Dip: | 240 / 72 | Direction: | ||
| Plunge: |
| Stratigraphic classification of host rock |
| Era: | Paleozoic | Period: | Ordovician |
| Province: | ||
| Geotec.unit: | ||
| Tectonic complex: | ||
| Igneous complex: |
| Group: | Ølve-Varaldsøykompl. | Formation: |
Mineralogy |
| Relationship | Mineral | Amount | |
| Gangue mineral | Quartz | Major mineral (>10%) | |
| Ore mineral | Pyrite | Subordinate mineral (1-10%) | |
| Ore mineral | Magnetite | Subordinate mineral (1-10%) |
Lithology: |
| Relationship | Rock | Origin | |
| Host rock | Skifrig grønnsten | Extrusive Original rock :Basalt |
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| Metamorphic facies :Greenschist |
Structures |
| Location: | Type: | Orientation(360 gr.): | Relation to min.: | |
| Host rock | Primary layering | Strike/Dip :240 / 72 | Syn-mineralisation ;...Effect :Controls |
Information(s) in free text format |
| Free text |
| Fra Sandvika må en gå 6-700 m på en smal sti mot Hisdalen inntil en ser en rustsone som ligger 20-30 m mot øst for stien. Ovenfor rustsonen ligger to 15 m lange stoller. Den øvre ligger 40-50 m over den nedre. Stollene er drevet inn i samme horisont og parallelt med lagdelingen og forskifringen. Ved begge stoller ses en 20-25 cm tykk mineralisert sone. Lokaliteten er uinteressant, og den ble ikke prøvetatt. |
Bibliography: |
| From NGU's Reference Archive: |
| Munster, C.A. , 1909 |
| Anvers. Sandvikfjeldets og Hisdalens skjærp. |
| ;Norges geologiske undersøkelse;FAGRAPPORT;Bergarkivet; No.BA 1865;1 pages |
| Abstract: | |
| Lok. Nr. 20276, 20281. Rapporten anbefaler undersøkelser ved disse 2 lokaliteter uten å gi geologiske opplysninger. |
| The fact sheet was created on 26.04.2024 |
| Questions or comments regarding the fact sheet can be emailed to: ressursdatabaser@ngu.no |
| Copyright © 2024 Geological Survey of Norway |