Norsk versjon | |||||
THE ORE DATABASE | |||||
Occurence 5546 - 047 Storvatnet | |||||
(Object Id: 1443) (Last updated: 09.02.2005) |
|
Location |
County: | Troms | Municipality: | Kvænangen (5546) |
Map 1:50000: | Øksfjordjøkulen (1735-2) | Map 1:250000: | Hammerfest |
Coordinate system: | EU89-UTM Zone 34 |
East: | 524085 m. | North: | 7778801 m. |
Longitude: | 21.6344750 | Latitude: | 70.1148080 |
Show on map |
|
Resource |
Resource Type: | Ferrous metals(Fe, Mn, Ti) | Resource Subtype: | Iron-Titanium | |
Element(s): | Fe Ti |
Importance |
Raw material meaning: | Little Importance (reg. 18.02.2015) |
Resources and production |
Activity: | Exploration | Reserves: | ||
Operating method: | Historical production: |
Mineralization |
Era: | Proterozoic | Period: | Paleoproterozoic | |
Genesis: | Form: | |||
Main texture: | Min. distribution: |
Main grain size: | Main alteration: |
Strike/Dip: | Direction: | |||
Plunge: |
Ti-deposit type(s) |
Main type: | Magmatic | Ilm/Mt-ratio: | ||
Sub type: | Mt +/- Ilm +/- Ap in mafic intrusion | %TiO(Ore): | ||
Titanium province: | Seiland | %P2O5(Ore): | ||
Host rock: | %MgO(Ilm): | |||
Main Ti mineral: | Ilmenite | %V2O3(Mt): | ||
ppm U (Rutile): |
Stratigraphic classification of host rock |
Era: | Proterozoic | Period: | Paleoproterozoic |
Province: | Barents Sea Region | |
Geotec.unit: | ||
Tectonic complex: | ||
Igneous complex: |
Group: | Formation: |
Mineralogy |
Relationship | Mineral | Amount | |
Gangue mineral | Plagioclase | Major mineral (>10%) | |
Gangue mineral | Pyroxene | Major mineral (>10%) | |
Gangue mineral | Amphibole | Subordinate mineral (1-10%) | |
Gangue mineral | Apatite | Accessory mineral (<1%) | |
Gangue mineral | Spinel | Accessory mineral (<1%) | |
Gangue mineral | Zircon | Accessory mineral (<1%) | |
Ore mineral | Magnetite | Major mineral (>10%) | |
Ore mineral | Ilmenite | Major mineral (>10%) |
Lithology: |
Relationship | Rock | Origin | |
Host rock | Gabbro | Intrusive Original rock :Gabbro |
Information(s) in free text format |
Free text |
I ura er det endel blokker nedrast fra stupet av en finkornet gabbroid bergart med ilmenitt-magnetitt-disseminasjon (prøve 01 og 02) og tildels semimassive oksydpartier. Mineraliseringen må opptre et sted i dette stupbratte fjellet, like ved kontakten til intruderende ultrabasitt, som i nærheten fører Ni-Cu-mineralisering (Småvatna og Bonjikdalen). Søyland Hansen (1971) har også funnet ilmenittanrikning med disseminerte sulfidkorn i en pyroksenittisk, gabbroid bergart SØ for Storvatnet (mineralisering 1). (Søyland Hansen benevner Storvatnet for Stålvatnet, hvilket var ukjent for lokalbefolkningen i Reinfjord.) |
Bibliography: |
From NGU's Reference Archive: |
Roberts, David , 1974 |
Hammerfest. Beskrivelse til det 1:250 000 berggrunnsgeologiske kart. (Med geologisk og aeromagnetisk kart) |
;Norges geologiske undersøkelse;TIDSSKRIFTARTIKKEL; KARTBESKRIVELSE;NGU; Skrifter; No.301; 10;1-66 + ka pages |
Abstract: | |
General descriptions of the different metasediments, metavolcanics and igneous rocks within the map area are presented. Three principal map-subdivisions are recognized; (a) supracrustal Precambrian (Karelian) rocks occurring in tectonic Windiws; (b) autochthonous late Precambrian to Lower Cambrian (meta)sediments; and (c) a thick allochthonous nappe-complex od Eocambrian to Cambrian metasediments, gneisses and various igneous rocks. In addition to these lithologies, sediments of unknown age (but possibly Silurian) lying unconformably upon allochthonous gneisses are noted from the south-western corner of the map-sheet. Descriptions are given of the many types of plutonic rocks occurring within the Seiland-Stjernøy petrographic province. These include several varieties of gabbro as well as diorites, peridotites, syenite, nepheline syenite, hornblendite, carbonatite, anorthosite, trondhjemite and adamellite. The major tectonic structural subdivisions of the map-area are outlined and it is shown that the matamorphic lithologies of the allochthon, here referred to as the Kalak nappe-complex, can be readily separated into three main tectonic units, or nappes. |
References not to be found in NGU's Reference Archive.: |
Søyland Hansen, T. 1971: En undersøkelse av nikkel-kopper mineraliseringer i Reinfjord-Jøkkelfjord området, Troms. Diplomoppg. NTH. |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||
TR0498.01 | Bedrock |
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TR0498.02 | Bedrock |
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NB! All analyse values are shown at the end of the printout.: |
Name of Locality: Skjerp 1 |
(Object Id: 1799 47,01,00) |
|
Location |
County: | Troms | Municipality: | Kvænangen (5546) |
Map 1:50000: | Øksfjordjøkulen (1735-2) | Map 1:250000: | Hammerfest |
Coordinate system: | EU89-UTM Zone 34 |
East: | 524645 m. | North: | 7778901 m. |
Longitude: | 21.6492540 | Latitude: | 70.1156510 |
Show on map |
|
Resource |
Resource Type: | Ferrous metals(Fe, Mn, Ti) | Resource Subtype: | Iron-Titanium | |
Element(s): | Fe Ti |
Resources and production |
Activity: | Exploration | Reserves: | ||
Operating method: | Historical production: |
Analyse Results |
from |
Deposit Area 5546 - 047 Storvatnet |
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# |
TR0498.01 | Bedrock | 78 | 8 | 3 | 21 | 46 | -.3 | -2.0 |
TR0498.02 | Bedrock | 109 | 10 | -3 | 39 | 79 | -.3 | -2.0 |
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Sample No. | Pt# | Pd# | Rh# | As* | Cd* | Ba* | Mo* | Sb* | Bi* |
TR0498.01 | -3.0 | -3.0 | -5.0 | 4 | -.2 | 17 | -1.00 | 4 | -2 |
TR0498.02 | -3.0 | -3.0 | -5.0 | 2 | -.2 | 5 | -1.00 | -2 | -2 |
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Sample No. | S% | V* | Cr* | Mn* | Fe% | Th* | U* | W* | Sr* |
TR0498.01 | .18 | 410 | 132 | 111 | 6.07 | -2.00 | -5.00 | -2 | 117.0 |
TR0498.02 | .28 | 632 | 384 | 165 | 9.31 | -2.00 | -5.00 | -2 | 34.0 |
------------------ |
Sample No. | La* | B* | |||||||
TR0498.01 | -1.00 | -3 | |||||||
TR0498.02 | -1.00 | -3 |
The fact sheet was created on 05.05.2024 |
Questions or comments regarding the fact sheet can be emailed to: ressursdatabaser@ngu.no |
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