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THE ???? DATABASE | |||||
Occurence 0 - 000 FEIL | |||||
(Object Id: ) (Last updated: 16.04.2020) |
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Location |
County: | Municipality: | Mangler () |
Map 1:50000: | Trondheim (1621-4) | Map 1:250000: | Trondheim |
Coordinate system: | UTM-Zone 33 - EUREF89/WGS84 |
East: | 584200 m. | North: | 7030260 m. |
Longitude: | 10.6865770 | Latitude: | 63.3912800 |
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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: | Pitting | Reserves: | ||
Operating method: | Historical production: |
Mineralization |
Era: | Paleozoic | Period: | Ordovician | |
Genesis: | Sedex | Form: | ||
Main texture: | Structureless | Min. distribution: | Disseminated (<20 % ore minerals) |
Main grain size: | Fine grained (< 1 mm) | Main alteration: | Chloritisation |
Strike/Dip: | 30 / 10 | Direction: | ||
Plunge: |
Stratigraphic classification of host rock |
Era: | Paleozoic | Period: | Ordovician |
Province: | Caledonides | |
Geotec.unit: | Trondheim Nappe Complex | |
Tectonic complex: | ||
Igneous complex: |
Group: | Formation: | Herjuan formation |
Mineralogy |
Relationship | Mineral | Amount | |
Gangue mineral | Quartz | Major mineral (>10%) | |
Gangue mineral | Mica | Subordinate mineral (1-10%) | |
Ore mineral | Pyrrhotite | Major mineral (>10%) | |
Ore mineral | Pyrite | Major mineral (>10%) |
Lithology: |
Relationship | Rock | Origin | |
Host rock | Quartz phyllite | Sedimentary Original rock :Argillaceous sediment |
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Metamorphic facies :Greenschist |
Structures |
Location: | Type: | Orientation(360 gr.): | Relation to min.: | |
Host rock | Schistosity | Strike/Dip :30 / 10 | Post-mineralisation ;...Effect :Modifies |
Information(s) in free text format |
Free text |
Bjørnberget ligger sør for Damvatnet. En 8 m lang, 2-3 m bred og opptil 2 m høy stoll er drevet mot sørøst (135°) i bunnen av brattskrenten på nordsida av Bjørnberget. Svak disseminasjon av magnetkis og pyritt finnes i mørk, skjærdeformert kvartsfyllitt med enkelte kvartslinser i cm-skala. Den tilnærmet flattliggende sonen kan følges i minst 30 m langs skrenten. Skrenten er gulfarget av svovelutfelling over en bredde på 7-8 m, men det er lite sulfider å se i fastfjell. |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||
JS97012 | Dump |
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JS97013 | Dump |
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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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