Norsk versjon | |||||
THE ORE DATABASE | |||||
Deposit Area 2017 - 002 | |||||
(Last updated 03.feb.2005) |
Name of Deposit Area : Indrevoll |
(Object Id : 2017,002,00,00) |
Location |
County : | Finnmark (20) | Municipality : | Kvalsund (2017) |
Map 1:50000: | Repparfjorden (1935-1) | Map 1:250000: | Honningsvåg |
Marking point: | Longitude: | 24.3336210 | Latitude: | 70.4310820 |
EU89-UTM Zone 34 | (Coordinates IS confirmed) |
X-coord: | 624562 m. | Y-coord: | 7817362 m. |
|
Commodity |
Main Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Sub Type: | Lead | |
Element(s): | Pb |
Production |
Activity: | Exploration | Reserves: | ||
Prod. method: | Production: | |||
Prod. status: | Volume of dump: |
Importance |
Public: | Little Importance (reg. 18.02.2015) |
Economical: | Minor interest , (Confirmed 03.feb.2005 by Peter Ihlen) |
Mineralization |
Era: | Proterozoic | Period: | Neoproterozoic | |
Dating: | Method: | |||
Genesis: | Sedex | Form: | Lens | |
Main texture: | Pore space filling | Min. distribution: | Disseminated (<20 % ore minerals) |
Main grain size: | Medium grained (1-3 mm) | Main alteration: |
Strike/Dip: | Direction: | |||
Plunge: |
Stratigraphic classification of host rock |
Era: | Proterozoic | Period: | Neoproterozoic |
Province: | Caledonides | |
Geotec.unit: | Platform Supergroup | |
Tectonic complex: | ||
Igneous complex: |
Group: | Formation: | Lomvann |
Mineralogy |
Relationship | Mineral | Amount | |
Gangue mineral | Quartz | Major mineral (>10%) | |
Gangue mineral | Feldspar | Major mineral (>10%) | |
Gangue mineral | Carbonate | Subordinate mineral (1-10%) | |
Gangue mineral | Muscovite | Subordinate mineral (1-10%) | |
Ore mineral | Pyrite | Major mineral (>10%) | |
Ore mineral | Galena | Major mineral (>10%) |
Lithology: |
Relationship | Rock | Origin | |
Host rock | Feltspatisk sandstein | Sedimentary Original rock :Arkosic sandstone |
|
Metamorphic facies :Zeolite |
Structures |
Location: | Type: | Orientation(360 gr.): | Relation to min.: | |
Host rock | Primary layering | Strike/Dip :35 / 70 | Post-mineralisation ;...Effect :Modifies |
Information(s) in free text format |
Free text |
Blyglansmineraliseringen opptrer i nedre del av Lomvannformasjonen nord for Raudfjell. En 10 m lang røskegrøft finnes på tvers av strøket. Lomvannformasjonen er svakt metamorfosert men kraftig foldet med åpne til tett folder med NØ-SV orienterte akser. Blyglans finnes disseminert i linseformede lag og i kvartsårer i kvartsittisk og feltspatisk sandstein og dels i konglomerat. De rikeste mineraliseringene er påvist i den 7 m mektige basalsonen. Forekomsten er dannet på tilsvarende måte som de andre fjellkjederandforekomstene, men blygalns er remobilisert inn på kvartsårer i sterkere grad. |
Bibliography: |
From NGU's Reference Archive: |
Pharaoh, Tim C.; Ramsey, Donald; Jansen, Øystein , 1983 |
Stratigraphy and structure of the northern part of the Repparfjord - Komagfjord window, Finnmark, Northern Norway. |
;Norges geologiske undersøkelse;TIDSSKRIFTARTIKKEL;NGU; No.377;1-45 pages |
Abstract: | |
In the northern district of the Repparfjord-Komagfjord Window, supracrustal and intrusive rocks of Early Proterozoic age are unconformably overlain by a thin sequence of Vendian sediments. Both of these units are overthrust by allochthonous rocks of the lavas, tuffs and sediments of the Raipas Supergroup and intrusions of the Raudfjell Suite, regionally metamorphosed at greenschist facies during the polyphase Svecokarelian Orogeny, c. 1840 Ma. The c. 8 km thick supracrustal sequence is divided into four groups and eleven formations on a lithostratigraphic basis. The lithological characteristics of these units are described and compared with rocks of similiar age elsewhere in N. Norway. The stratigraphy and sedimentology of the thin (<200 m thick), autochtonous, Vendian cover sequence is also described. The caledonian Orogeny resulted in complex deformation of the autochtonous cover as well as considerable reactiviation of the underlying basement. |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | |||||
JS85148 | Bedrock |
|
NB! All analyse values are shown at the end of the printout.: |
Analyse Results |
from |
Deposit Area 2017 - 002 Indrevoll |
Element analyses |
( *=parts pr. million, #=parts pr.billion, Negative values means below detection limit value.) |
Sample No. | Sample Type | Cu* | Zn* | Pb* | Ba* | Mo* | V* | Th* |
JS85148 | Bedrock | 3 | 40 | 1395 | 4060 | 3.00 | 39 | 8.00 |
------------------ |
Sample No. | Rb* | Sr* | Y* | Zr* | Nb* | ||||
JS85148 | 72.0 | 50.0 | 9.0 | 182 | 3.00 |
Oxide analyses |
( All values are in % ) |
Sample No. | Sample Type | SiO2 | Al2O3 | TiO2 | Fe2O3 | MnO | MgO | CaO |
JS85148 | Bedrock | 85.11 | 6.99 | 0.21 | 0.81 | 0.02 | 0.41 | 0.34 |
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Sample No. | Na2O | K2O | P2O5 | Loss | Sum | ||||
JS85148 | 1.22 | 3.57 | 0.01 | 0.58 | 99.00 |
The fact sheet was created on 18.05.2024 |
Questions or comments regarding the fact sheet can be emailed to: ressursdatabaser@ngu.no |
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