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THE ???? DATABASE | |||||
Occurence 0 - 000 FEIL | |||||
(Object Id: ) (Last updated: 08.05.2006) |
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Location |
County: | Municipality: | Mangler () |
Map 1:50000: | Kvikneskogen (1619-4) | Map 1:250000: | Røros |
Coordinate system: | UTM-Zone 33 - EUREF89/WGS84 |
East: | 582800 m. | North: | 6904790 m. |
Longitude: | 10.5963530 | Latitude: | 62.2659560 |
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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: | Little Importance (reg. 18.02.2015) |
Resources and production |
Activity: | Pitting | Reserves: | ||
Operating method: | Historical production: |
Operations |
From - To | Activity | Comments | |
Pitting | Company/Institution :? | ||
1998 - 1998 | Sampling | Company/Institution :NGU mineralressurser |
Mineralization |
Era: | Paleozoic | Period: | Ordovician | |
Genesis: | Volcex | Form: | ||
Main texture: | Banded | Min. distribution: | Disseminated (<20 % ore minerals) |
Main grain size: | Medium grained (1-3 mm) | Main alteration: | Sericitisation |
Strike/Dip: | Direction: | |||
Plunge: |
Stratigraphic classification of host rock |
Era: | Paleozoic | Period: | Ordovician |
Province: | Caledonides | |
Geotec.unit: | Trondheim Nappe Complex | |
Tectonic complex: | ||
Igneous complex: |
Group: | Fundsjø Group | Formation: |
Mineralogy |
Relationship | Mineral | Amount | |
Gangue mineral | Quartz | Major mineral (>10%) | |
Gangue mineral | Sericite | Major mineral (>10%) | |
Ore mineral | Pyrite | Major mineral (>10%) |
Lithology: |
Relationship | Rock | Origin | |
Wall rock | Chlorite schist | Sedimentary Original rock :Tuffite |
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Metamorphic facies :Greenschist | |||
Wall rock | Quartz keratophyre | Extrusive Original rock :Rhyodacite |
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Metamorphic facies :Greenschist |
Structures |
Location: | Type: | Orientation(360 gr.): | Relation to min.: | |
Wall rock | Foliation | Strike/Dip :200 / 80 | Post-mineralisation ;...Effect :Controls | |
Wall rock | Fold axis | Dir./Plunge :209 / 41 | Post-mineralisation ;...Effect :Modifies |
Information(s) in free text format |
Free text |
Skjerpet ligger ute på en stor myrlendt snauflate, like ved stien mellom Veslsætra og Liveslsætra og består av en 2x2 m røsk ca. 0.5 m dyp. Mineralisering består av meget svak pyrittimpregnasjon, dels anriket i tynne striper, som opptrer i sericittomvandlet kvarts-keratofyr/rhyodacitt. Pyritt opptrer typisk i subhedrale 1-2 mm korn. Det er utviklet en lineasjon som følge av småfolding i retning 209/41, mens foliasjonen har strøk 200/(0. Mineraliseringen her ligger innenfor den samme ekstensive omvandlingssonen som skjerpet Svartåsvangen (HE0119), som ligger ca. 600 m mot sør. |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||
HE0161.01 | Bedrock |
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NB! All analyse values are shown at the end of the printout.: |
The fact sheet was created on 02.05.2024 |
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