Norsk versjon | |||||
THE ORE DATABASE | |||||
Occurence 5006 - 007 Persgardshalla | |||||
(Object Id: 141) (Last updated: 15.05.2006) |
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Location |
County: | Trøndelag | Municipality: | Steinkjer (5006) |
Map 1:50000: | Snåsavatnet (1723-2) | Map 1:250000: | Namsos |
Coordinate system: | EU89-UTM Zone 32 |
East: | 633119 m. | North: | 7110592 m. |
Longitude: | 11.7316380 | Latitude: | 64.0962290 |
Show on map |
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Resource |
Resource Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Resource Subtype: | Copper | |
Element(s): | Cu Au |
Importance |
Raw material meaning: | Little Importance (reg. 18.02.2015) |
Resources and production |
Activity: | Pitting | Reserves: | ||
Operating method: | Historical production: |
Operations |
From - To | Activity | Comments | |
1990 - 1990 | Geophysics | Company/Institution :NGU |
Mineralization |
Genesis: | Hydrothermal vein | Form: | Irregular | |
Main texture: | Min. distribution: | Irregular (scattered) |
Main grain size: | Medium grained (1-3 mm) | Main alteration: |
Strike/Dip: | Direction: | |||
Plunge: |
Stratigraphic classification of host rock |
Era: | Period: |
Province: | ||
Geotec.unit: | ||
Tectonic complex: | ||
Igneous complex: |
Group: | Formation: |
Mineralogy |
Relationship | Mineral | Amount | |
Ore mineral | Chalcopyrite | Major mineral (>10%) | |
Ore mineral | Bornite | Major mineral (>10%) | |
Ore mineral | Pyrite | Subordinate mineral (1-10%) |
Bibliography: |
From NGU's Reference Archive: |
Dalsegg, Einar; Grenne, Tor , 1991 |
Persgardshalla Cu-Au mineralisering. IP-målinger og geologi Steinkjer, Nord-Trøndelag. |
;Norges geologiske undersøkelse;FAGRAPPORT;NGU-rapport; No.91.051;13 pages |
Abstract: | |
Rapporten beskriver resultatene fra geofysiske- og geologiske undersøkelser av Persgardshalla Cu-Au mineralisering ved Binde i Steinkjer kommune. Undersøkelsene har vist at mineraliseringene ved Persgardhalla er helt lokale kobber-gull-anrikninger uten noen økonomisk interesse. Det er ingen antydning til andre gullanrikninger i området. IP-målingene tyder ikke på noen ut- bredelse av sulfidmineraliseringer av betydning langs N-S strukturer. De IP- anomaliene som er registrert er trolig relatert til Ø-V strykende, lag- formige Fe-sulfiddisseminasjoner uten noen edelmetall- eller basemetall- anrikning. |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||
TG90017 | Bedrock |
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TG90018 | Bedrock |
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TG90019 | Bedrock |
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TG90020 | Bedrock |
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TG90021 | Bedrock |
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TG90022 | Bedrock |
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TG90113 | Bedrock |
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TG90114 | Bedrock |
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TG90115 | Bedrock |
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TG90116 | Bedrock |
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TG90117 | Bedrock |
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TG90118 | Bedrock |
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TG90119 | Bedrock |
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TG90120 | Bedrock |
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TG90121 | Bedrock |
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TG90122 | Bedrock |
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TG90123 | Bedrock |
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TG90124 | Bedrock |
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TG90125 | Bedrock |
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TG90126 | Bedrock |
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TG90127 | Bedrock |
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NB! All analyse values are shown at the end of the printout.: |
Analyse Results |
from |
Deposit Area 5006 - 007 Persgardshalla |
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# |
TG90017 | Bedrock | 84 | 29 | 10 | 19 | 45 | .5 | 3.0 |
TG90018 | Bedrock | 162 | 4 | 3 | 5 | 43 | .3 | 3.0 |
TG90019 | Bedrock | 30 | 16 | 9 | 2 | 4 | .2 | 2.0 |
TG90020 | Bedrock | 122 | 41 | 7 | 11 | 31 | .3 | 1.0 |
TG90021 | Bedrock | 53 | 22 | 7 | 2 | 5 | .2 | 1.0 |
TG90022 | Bedrock | 71 | 104 | 27 | 6 | 36 | .4 | 2.0 |
TG90113 | Bedrock | 1158 | 163 | 4 | 42 | 72 | 2.1 | 570.0 |
TG90114 | Bedrock | 1225 | 1 | 9 | 2 | 3 | 4.4 | 478.0 |
TG90115 | Bedrock | 6905 | 1 | 4 | 1 | 4 | 11.3 | 1833.0 |
TG90116 | Bedrock | 94 | 3 | 2 | 1 | 3 | .1 | 13.0 |
TG90117 | Bedrock | 215 | 81 | 12 | 23 | 47 | .3 | 31.0 |
TG90118 | Bedrock | 172 | 97 | 8 | 26 | 62 | .2 | 22.0 |
TG90119 | Bedrock | 156 | 3 | 2 | 1 | 4 | .2 | 41.0 |
TG90120 | Bedrock | 1502 | 100 | 12 | 26 | 53 | 1.4 | 345.0 |
TG90121 | Bedrock | 8118 | 1 | 3 | 2 | 6 | 19.3 | 3333.0 |
TG90122 | Bedrock | 3623 | 6 | 4 | 2 | 6 | 7.3 | 1603.0 |
TG90123 | Bedrock | 12049 | 1 | 10 | 5 | 10 | 34.0 | 5730.0 |
TG90124 | Bedrock | 4563 | 5 | 12 | 3 | 2 | 3.5 | 524.0 |
TG90125 | Bedrock | 2083 | 1 | 2 | 2 | 5 | 3.4 | 359.0 |
TG90126 | Bedrock | 2855 | 4 | 3 | 4 | 9 | 2.2 | 263.0 |
TG90127 | Bedrock | 19207 | 1 | 3 | 2 | 4 | 29.4 | 1609.0 |
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Sample No. | Pt# | Pd# | Rh# | As* | Cd* | Ba* | Mo* | Sb* | Bi* |
TG90017 | 1.0 | 3.0 | 3.0 | 11 | .5 | 72 | 5.00 | 2 | 2 |
TG90018 | 1.0 | 3.0 | 2.0 | 8 | .2 | 25 | 13.00 | 6 | 2 |
TG90019 | 1.0 | 2.0 | 2.0 | 7 | .2 | 36 | 1.00 | 3 | 2 |
TG90020 | 1.0 | 4.0 | 2.0 | 4 | .2 | 71 | 1.00 | 3 | 2 |
TG90021 | 1.0 | 2.0 | 2.0 | 2 | .2 | 45 | 1.00 | 3 | 2 |
TG90022 | 1.0 | 3.0 | 2.0 | 3 | .4 | 145 | 7.00 | 3 | 2 |
TG90113 | 1.0 | 2.0 | 2.0 | 26 | .5 | 419 | 1.00 | 2 | 2 |
TG90114 | 1.0 | 3.0 | 2.0 | 8 | .7 | 3 | 1.00 | 3 | 2 |
TG90115 | 1.0 | 2.0 | 2.0 | 8 | .5 | 9 | 1.00 | 3 | 2 |
TG90116 | 1.0 | 3.0 | 2.0 | 2 | .2 | 2 | 1.00 | 3 | 4 |
TG90117 | 3.0 | 6.0 | 4.0 | 4 | .5 | 160 | 1.00 | 2 | 2 |
TG90118 | 1.0 | 2.0 | 2.0 | 13 | .2 | 447 | 1.00 | 2 | 2 |
TG90119 | 1.0 | 2.0 | 2.0 | 2 | .2 | 13 | 1.00 | 2 | 2 |
TG90120 | 1.0 | 2.0 | 2.0 | 4 | 1.0 | 141 | 1.00 | 2 | 3 |
TG90121 | 1.0 | 2.0 | 2.0 | 3 | .8 | 8 | 1.00 | 2 | 2 |
TG90122 | 2.0 | 3.0 | 2.0 | 2 | .4 | 8 | 1.00 | 2 | 2 |
TG90123 | 2.0 | 6.0 | 5.0 | 3 | 1.9 | 16 | 1.00 | 2 | 4 |
TG90124 | 1.0 | 2.0 | 2.0 | 8 | 1.6 | 6 | 1.00 | 3 | 2 |
TG90125 | 1.0 | 2.0 | 2.0 | 2 | .2 | 11 | 1.00 | 3 | 2 |
TG90126 | 3.0 | 2.0 | 2.0 | 2 | .8 | 9 | 1.00 | 3 | 2 |
TG90127 | 1.0 | 2.0 | 2.0 | 9 | 1.6 | 2 | 1.00 | 2 | 2 |
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Sample No. | S% | V* | Cr* | Mn* | Fe% | Th* | U* | W* | Sr* |
TG90017 | 2.14 | 63 | 39 | 1081 | 4.90 | 3.00 | 5.00 | 1 | 273.0 |
TG90018 | .15 | 18 | 7 | 75 | 4.44 | 2.00 | 5.00 | 1 | 12.0 |
TG90019 | .18 | 3 | 2 | 214 | 2.36 | 13.00 | 5.00 | 1 | 36.0 |
TG90020 | .17 | 22 | 23 | 783 | 3.20 | 8.00 | 5.00 | 1 | 15.0 |
TG90021 | .24 | 11 | 3 | 52 | 2.34 | 15.00 | 5.00 | 1 | 55.0 |
TG90022 | .17 | 27 | 8 | 369 | 3.09 | 14.00 | 5.00 | 1 | 40.0 |
TG90113 | .01 | 76 | 50 | 490 | 5.72 | 1.00 | 6.00 | 1 | 93.0 |
TG90114 | .03 | 2 | 4 | 45 | .60 | 5.00 | 5.00 | 2 | 3.0 |
TG90115 | .22 | 2 | 4 | 108 | .50 | 1.00 | 5.00 | 2 | 32.0 |
TG90116 | .01 | 5 | 5 | 34 | .50 | 1.00 | 5.00 | 2 | 1.0 |
TG90117 | .02 | 58 | 55 | 896 | 4.24 | 1.00 | 5.00 | 1 | 410.0 |
TG90118 | .02 | 85 | 92 | 401 | 4.53 | 2.00 | 5.00 | 1 | 184.0 |
TG90119 | .02 | 3 | 5 | 35 | .40 | 1.00 | 5.00 | 2 | 9.0 |
TG90120 | .15 | 61 | 60 | 779 | 5.07 | 2.00 | 5.00 | 1 | 329.0 |
TG90121 | .37 | 2 | 5 | 164 | .69 | 1.00 | 5.00 | 2 | 58.0 |
TG90122 | .17 | 3 | 5 | 112 | .66 | 1.00 | 5.00 | 2 | 47.0 |
TG90123 | .72 | 4 | 5 | 1346 | 1.41 | 1.00 | 5.00 | 1 | 560.0 |
TG90124 | .46 | 1 | 1 | 2380 | 1.47 | 1.00 | 5.00 | 1 | 954.0 |
TG90125 | .15 | 1 | 4 | 116 | .57 | 1.00 | 5.00 | 2 | 27.0 |
TG90126 | .24 | 1 | 3 | 258 | .72 | 1.00 | 5.00 | 2 | 78.0 |
TG90127 | 1.22 | 1 | 4 | 37 | 1.33 | 1.00 | 5.00 | 2 | 4.0 |
------------------ |
Sample No. | La* | B* | |||||||
TG90017 | 2.00 | 3 | |||||||
TG90018 | 2.00 | 5 | |||||||
TG90019 | 38.00 | 5 | |||||||
TG90020 | 16.00 | 6 | |||||||
TG90021 | 60.00 | 6 | |||||||
TG90022 | 35.00 | 4 | |||||||
TG90113 | 2.00 | 2 | |||||||
TG90114 | 2.00 | 3 | |||||||
TG90115 | 2.00 | 3 | |||||||
TG90116 | 2.00 | 3 | |||||||
TG90117 | 7.00 | 2 | |||||||
TG90118 | 7.00 | 2 | |||||||
TG90119 | 2.00 | 4 | |||||||
TG90120 | 9.00 | 2 | |||||||
TG90121 | 2.00 | 3 | |||||||
TG90122 | 2.00 | 3 | |||||||
TG90123 | 2.00 | 4 | |||||||
TG90124 | 2.00 | 2 | |||||||
TG90125 | 2.00 | 2 | |||||||
TG90126 | 2.00 | 2 | |||||||
TG90127 | 2.00 | 2 |
The fact sheet was created on 20.04.2024 |
Questions or comments regarding the fact sheet can be emailed to: ressursdatabaser@ngu.no |
Copyright © 2024 Geological Survey of Norway |