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THE ???? DATABASE | |||||
Occurence 0 - 000 FEIL | |||||
(Object Id: ) (Last updated: 08.11.2019) |
Belongs to the Province: Fossum Jernverk |
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Location |
County: | Municipality: | Mangler () |
Map 1:50000: | Nordagutu (1713-4) | Map 1:250000: | Skien |
County: | UTM-Zone 33 - EUREF89/WGS84 |
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Resource |
Resource Type: | Ferrous metals(Fe, Mn, Ti) | Resource Subtype: | Iron | |
Element(s): | Fe Mn |
Importance |
Raw material meaning: | Not Assessed (reg. 18.02.2015) |
Resources and production |
Activity: | Pitting | Reserves: | ||
Operating method: | Historical production: |
Mineralization |
Era: | Paleozoic | Period: | Permian | |
Genesis: | Hydrothermal vein | Form: | ||
Main texture: | Min. distribution: |
Main grain size: | Main alteration: |
Strike/Dip: | 308 / 90 | Direction: | ||
Plunge: |
Stratigraphic classification of host rock |
Era: | Proterozoic | Period: | Mesoproterozoic |
Province: | South Norwegian Basement Province | |
Geotec.unit: | ||
Tectonic complex: | ||
Igneous complex: |
Group: | Formation: |
Mineralogy |
Relationship | Mineral | Amount | |
Gangue mineral | Garnet | Major mineral (>10%) | |
Gangue mineral | Epidote | Major mineral (>10%) | |
Gangue mineral | Quartz | Major mineral (>10%) | |
Gangue mineral | Hornblende | Subordinate mineral (1-10%) | |
Ore mineral | Magnetite | Major mineral (>10%) |
Lithology: |
Relationship | Rock | Origin | |
Wall rock | Granite | Intrusive Original rock :Granite |
Structures |
Location: | Type: | Orientation(360 gr.): | Relation to min.: | |
Wall rock | Foliation | Strike/Dip :307 / 70 | Pre-mineralisation ;...Effect :None |
Information(s) in free text format |
Free text |
Det befinner seg to mindre grøfter på Bjørndalsåsen. Her skal det også være en sulfidforekomst som kalles Skridua (TE 0394). Denne ble imidlertid ikke funnet. Det som regnes som hovedgruva er en 15 m lang grøft i tilnærmet Ø-V retning (308 grader). Den er 1m bred og 1-3 m dyp (dypest i vest). Det er svært lite mineralisert materiale å finne. Blokker består av drusekvarts med kun spredte korn av magnetitt. Ellers er det dels noe epidot og rødbrun granat. Om lag 80 m mot SV er en ca. 10 m lang vannfylt grøft i Ø-V retning (090 grader). Mineralisering består av enkelte små aggregater av magnetitt i tett amfibol-epidot-granat matriks. Granatene er 2-3 mm store er gule til grønne, dels euhedrale krystaller. |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||
TE0423.02 | Dump |
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NB! All analyse values are shown at the end of the printout.: |
Name of Locality: Skjerp 1 |
(Object Id: 19107 52,01,00) |
|
Location |
County: | Municipality: | Mangler () |
Map 1:50000: | Nordagutu (1713-4) | Map 1:250000: | Skien |
County: | UTM-Zone 33 - EUREF89/WGS84 |
|
Resource |
Resource Type: | Ferrous metals(Fe, Mn, Ti) | Resource Subtype: | Iron-Titanium | |
Element(s): |
Resources and production |
Activity: | Pitting | Reserves: | ||
Operating method: | Historical production: |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||
TE0423.01 | Dump |
|
NB! All analyse values are shown at the end of the printout.: |
Name of Locality: Skjerp 2 |
(Object Id: 19108 52,02,00) |
|
Location |
County: | Municipality: | Mangler () |
Map 1:50000: | Nordagutu (1713-4) | Map 1:250000: | Skien |
County: | UTM-Zone 33 - EUREF89/WGS84 |
|
Resource |
Resource Type: | Ferrous metals(Fe, Mn, Ti) | Resource Subtype: | Iron-Titanium | |
Element(s): |
Name of Locality: Skjerp 3 |
(Object Id: 19109 52,03,00) |
|
Location |
County: | Municipality: | Mangler () |
Map 1:50000: | Nordagutu (1713-4) | Map 1:250000: | Skien |
County: | UTM-Zone 33 - EUREF89/WGS84 |
|
Resource |
Resource Type: | Ferrous metals(Fe, Mn, Ti) | Resource Subtype: | Iron-Titanium | |
Element(s): |
Name of Locality: Skjerp 4 |
(Object Id: 19110 52,04,00) |
|
Location |
County: | Municipality: | Mangler () |
Map 1:50000: | Nordagutu (1713-4) | Map 1:250000: | Skien |
County: | UTM-Zone 33 - EUREF89/WGS84 |
|
Resource |
Resource Type: | Ferrous metals(Fe, Mn, Ti) | Resource Subtype: | Iron-Titanium | |
Element(s): |
The fact sheet was created on 26.04.2024 |
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