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THE ???? DATABASE | |||||
Occurence 0 - 000 FEIL | |||||
(Object Id: ) (Last updated: 30.10.2001) |
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Location |
County: | Municipality: | Mangler () |
Map 1:50000: | Dalsbygda (1620-2) | Map 1:250000: | Røros |
Coordinate system: | UTM-Zone 33 - EUREF89/WGS84 |
East: | 611650 m. | North: | 6956770 m. |
Longitude: | 11.1854730 | Latitude: | 62.7246750 |
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): | Fe sulphide |
Importance |
Raw material meaning: | Little Importance (reg. 18.02.2015) |
Resources and production |
Activity: | Pitting | Reserves: | ||
Operating method: | Historical production: |
Products |
Element/product | Crude ore grade or quality | Reg. date | |
Kis | 20.04.1998 |
Operations |
From - To | Activity | Comments | |
Pitting | |||
1997 - 1997 | Sampling | Company/Institution :NGU |
Mineralization |
Era: | Paleozoic | Period: | Ordovician | |
Genesis: | Volcex | Form: | Irregular | |
Main texture: | Banded | Min. distribution: | Disseminated (<20 % ore minerals) |
Main grain size: | Fine grained (< 1 mm) | Main alteration: | Chloritisation |
Strike/Dip: | Direction: | |||
Plunge: |
Stratigraphic classification of host rock |
Era: | Paleozoic | Period: | Ordovician |
Province: | Caledonides | |
Geotec.unit: | Trondheim Nappe Complex | |
Tectonic complex: | Meråker Nappe | |
Igneous complex: |
Group: | Fundsjø Group | Formation: |
Mineralogy |
Relationship | Mineral | Amount | |
Gangue mineral | Chlorite | Major mineral (>10%) | |
Gangue mineral | Quartz | Subordinate mineral (1-10%) | |
Ore mineral | Pyrite | Major mineral (>10%) |
Lithology: |
Relationship | Rock | Origin | |
Wall rock | Metagabbro | Intrusive Original rock :Gabbro |
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Metamorphic facies :Greenschist |
Structures |
Location: | Type: | Orientation(360 gr.): | Relation to min.: | |
Wall rock | Foliation | Strike/Dip :207 / 33 | Post-mineralisation ;...Effect :Controls |
Information(s) in free text format |
Free text |
Liten røsk (sprengning) i skrent ved skoggrensa rett øst for Hessjøen og under fjellknausen Kneppan. Røsken er et ca. 1 m dypt og 1m bredt innhugg i skrenten. Mineraliseringen består av svak pyritt-impregnasjon (ca. 5 % sulfider) i mm-laminert kvarts-klorittskifer. Pyrittkornene er <= 1 mm store og opptrer assosiert med kvarts, dels anriket i mm-tykke bånd. Sidebergarten er en finkornet metadiabas/-gabbro. |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||
ST0402.01 | Dump |
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NB! All analyse values are shown at the end of the printout.: |
The fact sheet was created on 23.04.2024 |
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