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Occurence 0 - 000 FEIL | |||||
(Object Id: ) (Last updated: 23.04.2015) |
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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: | 608770 m. | North: | 6950610 m. |
Longitude: | 11.1252170 | Latitude: | 62.6702900 |
Show on map |
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Resource |
Resource Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Resource Subtype: | Zinc | |
Element(s): | Kis Zn Cu Pb |
Importance |
Raw material meaning: | Not Assessed (reg. 20.03.2017) |
Resources and production |
Activity: | Test mining | Reserves: | 3500 thousand tons | |
Operating method: | Open pit and underground mining | Historical production: | -1 thousand tons |
Products |
Element/product | Crude ore grade or quality | Reg. date | |
Cu | 28.11.1997 | ||
Kis | 28.11.1997 |
Operations |
From - To | Activity | Comments | |
1830 - 1830 | Test mining | Company/Institution :Røros Kobberverk | |
Drift på kobber | |||
1905 - 1905 | Test mining | Company/Institution :Røros Kobberverk | |
Pyritt | |||
1948 - 1948 | Geophysics | Company/Institution :Geofysisk Malmleting | |
Turam bakkemålinger | |||
1974 - 1974 | Core drilling | Company/Institution :AS Sydvaranger | |
3 hull over E-anomalien | |||
1974 - 1974 | Geophysics | Company/Institution :NGU | |
Helikoptermålinger, EM | |||
1975 - 1976 | Geophysics | Company/Institution :NGU | |
SP og VLF bakkemålinger |
Mineralization |
Era: | Paleozoic | Period: | Ordovician | |
Genesis: | Volcex | Form: | Plate | |
Main texture: | Banded | Min. distribution: | Massive (>50 % ore minerals) |
Main grain size: | Fine grained (< 1 mm) | Main alteration: | Chloritisation |
Strike/Dip: | 200 / 60 | Direction: | ||
Plunge: |
Stratigraphic classification of host rock |
Era: | Paleozoic | Period: | Ordovician |
Province: | Caledonides | |
Geotec.unit: | Trondheim Nappe Complex | |
Tectonic complex: | Meråkerdekket | |
Igneous complex: |
Group: | Fundsjø | Formation: |
Mineralogy |
Relationship | Mineral | Amount | |
Gangue mineral | Chlorite | Major mineral (>10%) | |
Gangue mineral | Quartz | Major mineral (>10%) | |
Gangue mineral | Amphibole | Accessory mineral (<1%) | |
Ore mineral | Pyrite | Major mineral (>10%) | |
Ore mineral | Chalcopyrite | Subordinate mineral (1-10%) | |
Ore mineral | Sphalerite | Subordinate mineral (1-10%) | |
Ore mineral | Pyrrhotite | Subordinate mineral (1-10%) |
Lithology: |
Relationship | Rock | Origin | |
Wall rock | Greenstone | Extrusive Original rock :Basalt |
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Metamorphic facies :Greenschist |
Structures |
Location: | Type: | Orientation(360 gr.): | Relation to min.: | |
Wall rock | Foliation | Strike/Dip :201 / 58 | Post-mineralisation ;...Effect :Modifies | |
Wall rock | Fold axis | Dir./Plunge :257 / 54 | Post-mineralisation ;...Effect :Modifies |
Information(s) in free text format |
Free text |
The Nygruva mine consists of an excavation in a small hillside, and two minor shafts. The excavation is 3-4 m across strike towards the west, before in turns to the north and follows a 1 meter thick zone of massive, fine-grained diffusely banded pyrite ore with subordinate sphalerite. The ore zone wedges out in both directions along strike, but may continue downwards along the strongly defined lineation/fold axis. In the footwall are numerous bands and lenses of disseminated to semimassive pyrite in quartz. One sample from the dump contained 1.71% Cu and 3.01% Zn. The closest shaft is about 70 m to the north. Here are two thin zones (20 and 80 cm wide) of massive, banded pyrite mineralization. Two samples contained 1.32 and 1.43% Cu and 0.99 and 7.94% Zn, respectively. The second shaft is another 70 m to the north. Here a sample of massive pyrrhotite ore with subordinate chalcopyrite and pyrite contained 1.76% Cu and 0.81% Zn. In all the samples from the Nygruva mine, the contents of Pb, Ag and Au were extremely low (highest values were 24 ppm Pb, 4 ppm Ag and 0.1 ppm Au). Three holes were drilled in 1974, guided by a weak EM anomaly associated with the outcropping mineralization. Hole no. 301 intersected 0.25 m with 3.00% Cu and 0.50% Zn, while holes no.302 and 303 intersected only weak pyrite impregnation. |
Bibliography: |
References not to be found in NGU's Reference Archive.: |
Se under Hesjø gruve (ST0188) |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||
ST0196.01 | Dump |
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ST0196.02 | Dump |
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ST0196.03 | Dump |
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ST0196.04 | Dump |
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NB! All analyse values are shown at the end of the printout.: |
Name of Locality: Pit |
(Object Id: 32686 7,01,00) |
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Location |
County: | Municipality: | Mangler () |
Map 1:50000: | Dalsbygda (1620-2) | Map 1:250000: | Røros |
County: | UTM-Zone 33 - EUREF89/WGS84 |
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Resource |
Resource Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Resource Subtype: | Zinc | |
Element(s): | Kis Zn Cu Pb |
Name of Locality: Pit |
(Object Id: 32687 7,02,00) |
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Location |
County: | Municipality: | Mangler () |
Map 1:50000: | Dalsbygda (1620-2) | Map 1:250000: | Røros |
County: | UTM-Zone 33 - EUREF89/WGS84 |
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Resource |
Resource Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Resource Subtype: | Zinc | |
Element(s): | Kis Zn Cu Pb |
The fact sheet was created on 19.04.2024 |
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