Norsk versjon | |||||
THE ORE DATABASE | |||||
Deposit Area 1740 - 009 | |||||
(Last updated 16.mai.2006) |
Name of Deposit Area : Grønndalselv |
(Object Id : 1740,009,00,00) |
Location |
County : | Nord-Trøndelag (17) | Municipality : | Namsskogan (1740) |
Map 1:50000: | Skorovatn (1824-2) | Map 1:250000: | Grong |
Marking point: | Longitude: | 12.9182110 | Latitude: | 64.6530310 |
EU89-UTM Zone 33 | (Coordinates IS confirmed) |
X-coord: | 400572 m. | Y-coord: | 7171419 m. |
|
Commodity |
Main Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Sub Type: | Copper | |
Element(s): | Cu Kis |
Production |
Activity: | Pitting | Reserves: | ||
Prod. method: | Production: | |||
Prod. status: | Volume of dump: | 2 m3 |
Importance |
Public: | Little Importance (reg. 18.02.2015) |
Economical: | Minor interest |
Operations |
From - To | Activity | Comments | |
1969 - 1969 | Geophysics | Company/Institution :NGU | |
1970 - 1970 | Geophysics | Company/Institution :NGU | |
1974 - 1975 | Geophysics | Company/Institution :Grong Gruber | |
1977 - 1977 | Geology | Company/Institution :Grong Gruber A/S | |
1978 - 1978 | Geophysics | Company/Institution :Grong Gruber A/S | |
1981 - 1981 | Geophysics | Company/Institution :Grong Gruber A/S | |
1984 - 1984 | Geophysics | Company/Institution :Grong Gruber A/S | |
1994 - 1994 | Geology | Company/Institution :NGU | |
1996 - 1996 | Sampling | Company/Institution :NGU |
Mineralization |
Era: | Paleozoic | Period: | Ordovician | |
Dating: | Method: | |||
Genesis: | Volcex | Form: | Layer | |
Main texture: | Structureless | Min. distribution: | Disseminated (<20 % ore minerals) |
Main grain size: | Medium grained (1-3 mm) | Main alteration: | Silicification |
Strike/Dip: | 245 / 60 | Direction: | ||
Plunge: |
Stratigraphic classification of host rock |
Era: | Paleozoic | Period: | Ordovician |
Province: | Caledonides | |
Geotec.unit: | Køli Nappe Complex | |
Tectonic complex: | Gjersvik Nappe | |
Igneous complex: |
Group: | Gjersvik | Formation: |
Mineralogy |
Relationship | Mineral | Amount | |
Gangue mineral | Quartz | Major mineral (>10%) | |
Gangue mineral | Amphibole | Subordinate mineral (1-10%) | |
Gangue mineral | Mica | Subordinate mineral (1-10%) | |
Gangue mineral | Plagioclase | Subordinate mineral (1-10%) | |
Ore mineral | Pyrite | Major mineral (>10%) | |
Ore mineral | Pyrrhotite | Major mineral (>10%) | |
Ore mineral | Chalcopyrite | Subordinate mineral (1-10%) | |
Ore mineral | Sphalerite | Accessory mineral (<1%) |
Lithology: |
Relationship | Rock | Origin | |
Host rock | Quartz kerophyre | Extrusive Original rock :Rhyodacite |
|
Metamorphic facies :Greenschist | |||
Wall rock | Greenstone | Extrusive Original rock :Basalt |
|
Metamorphic facies :Greenschist |
Structures |
Location: | Type: | Orientation(360 gr.): | Relation to min.: | |
Host rock | Fold axis | Strike/Dip :66 / 50 | Post-mineralisation ;...Effect :Modifies | |
Wall rock | Foliation | Strike/Dip :245 / 60 | Post-mineralisation ;...Effect :Modifies |
Information(s) in free text format |
Free text |
Forekomsten ligger ca. 100 m NØ for Grønndalselva, ca. 800 m før dennes samløp med Skorovas-elva. Mineraliseringen ligger i amfibolittisk grønnstein i veksling med keratofyr og intermediære vulkanitter. Malmsonen stryker NØ/SV med steilt fall mot NV. Den er opptil 1 m mektig sentralt i skjerpet. Denne fortykning skyldes foldning og den kiler raskt ut langs strøket etter få meter. Mineraliseringen består av disseminert magnetkis, svovelkis og kobberkis i kvartsrik bergart, antatt silifisert keratofyr. I det sørøstligste skjerpet dominerer felsisk metavulkanitt. Ifølge geofysiske målinger har forekomsten ubetydelig utstrekning. |
Bibliography: |
From NGU's Reference Archive: |
Oftedahl, Christoffer , 1958 |
Oversikt over Grongfeltets skjerp og malmforekomster. |
;Norges geologiske undersøkelse;TIDSSKRIFTARTIKKEL;NGU; No.202;1-75 + fo pages |
Abstract: | |
Ore occurences of the Grong area: In the period 1910-1918 a great number of ore occurences were discovered in the Grong area. The late state geologist Steinar Foslie mapped the area in the years 1922-1931. Foslie also mapped all claims and occurences and made special field investigations in a few cases. This book presents a survey of all occurences chiefly based on the field observations of Foslie. In addition the present author has done some field work in connection with the three large deposits, Joma, Skorovass, and Gjersvik. The map, Plate 1, shows the areal geology and the location of the occurrences, numbered from 1 to 131. the ore of the occurrences is chiefly pyrite. The larger occurrences also contain some chalcopyrite and sphalerite etc. and the smaller occurrences contain ither pure pyrite with some magnetite. The Joma deposit (No. 1), contains about 15.5 mill. tons of ore. The ore zone forms an arc and is situated within a thick series of greenstones (Fig. 1). The Skorovass mine (No. 2), contains about 7,5 mill. tons of ore. The deposit is situated in a greenstone complex (Fig. 7), and is immediately surrounded by asid tuffs of quartz keratophyric composition (Table 1). |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||
NT0259.01 | Dump |
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NT0259.02 | Dump |
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NT0259.03 | Dump |
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NT0259.04 | Dump |
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NB! All analyse values are shown at the end of the printout.: |
Name of Locality : Grønndalselv Ø |
(Object Id : 1740,009,01,00) |
Location |
County : | Nord-Trøndelag (17) | Municipality : | Namsskogan (1740) |
Map 1:50000: | Skorovatn (1824-2) | Map 1:250000: | Grong |
Marking point: | Longitude: | 12.9186570 | Latitude: | 64.6526780 |
EU89-UTM Zone 33 | (Coordinates IS confirmed) |
X-coord: | 400592 m. | Y-coord: | 7171379 m. |
|
Commodity |
Main Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Sub Type: | Copper | |
Element(s): | Cu Kis |
Production |
Activity: | Pitting | Reserves: | ||
Prod. method: | Production: | |||
Prod. status: | Volume of dump: |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||
NT0259.05 | Dump |
|
||||
NT0259.06 | Dump |
|
NB! All analyse values are shown at the end of the printout.: |
Analyse Results |
from |
Deposit Area 1740 - 009 Grønndalselv |
Element analyses |
( *=parts pr. million, #=parts pr.billion, Negative values means below detection limit value.) |
Sample No. | Sample Type | Cu* | Zn* | Pb* | Co* | Ni* | Ag* | Au# |
NT0259.01 | Dump | 2076 | 196 | 11 | 49 | 93 | .9 | 12.0 |
NT0259.02 | Dump | 3624 | 334 | 21 | 80 | 182 | 1.5 | 14.0 |
NT0259.03 | Dump | 578 | 637 | 13 | 78 | 53 | -.3 | 11.0 |
NT0259.04 | Dump | 1742 | 300 | 15 | 56 | 108 | .7 | 8.0 |
NT0259.05 | Dump | 4678 | 64445 | 677 | 3 | 10 | 10.2 | 142.0 |
NT0259.06 | Dump | 86 | 261 | 181 | 2 | 2 | 1.3 | 10.0 |
------------------ |
Sample No. | Pt# | Pd# | Rh# | As* | Cd* | Ba* | Mo* | Sb* | Bi* |
NT0259.01 | -1.0 | -1.0 | -1.0 | -2 | -.2 | 2 | 5.00 | -2 | 5 |
NT0259.02 | -1.0 | 4.0 | -1.0 | 2 | -.2 | 5 | -1.00 | -2 | -2 |
NT0259.03 | 2.0 | 2.0 | -1.0 | 3 | .7 | 3 | 12.00 | -2 | -2 |
NT0259.04 | -1.0 | 1.0 | -1.0 | 2 | -.2 | 4 | 3.00 | -2 | 6 |
NT0259.05 | -1.0 | 1.0 | -1.0 | -2 | 234.8 | 12 | 53.00 | 2 | 8 |
NT0259.06 | -1.0 | 3.0 | 1.0 | -2 | .4 | 27 | -1.00 | -2 | -2 |
------------------ |
Sample No. | S% | V* | Cr* | Mn* | Fe% | Th* | U* | W* | Sr* |
NT0259.01 | 5.99 | 12 | 8 | 404 | 10.26 | -2.00 | -5.00 | -2 | 3.0 |
NT0259.02 | 9.80 | 27 | 16 | 1124 | 16.91 | -2.00 | -5.00 | -2 | 4.0 |
NT0259.03 | 4.81 | 105 | 262 | 2844 | 11.12 | -2.00 | -5.00 | -2 | 4.0 |
NT0259.04 | 6.78 | 27 | 14 | 860 | 10.38 | -2.00 | -5.00 | -2 | 3.0 |
NT0259.05 | 7.25 | 11 | 3 | 304 | 6.39 | -2.00 | -5.00 | 30 | 7.0 |
NT0259.06 | 1.22 | 5 | 1 | 660 | 2.45 | 5.00 | -5.00 | -2 | 9.0 |
------------------ |
Sample No. | La* | B* | |||||||
NT0259.01 | 3.00 | -3 | |||||||
NT0259.02 | 6.00 | -3 | |||||||
NT0259.03 | 2.00 | -3 | |||||||
NT0259.04 | 4.00 | -3 | |||||||
NT0259.05 | 4.00 | -3 | |||||||
NT0259.06 | 11.00 | -3 |
The fact sheet was created on 20.01.2025 |
Questions or comments regarding the fact sheet can be emailed to: ressursdatabaser@ngu.no |
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