Norsk versjon
THE INDUSTRIAL MINERAL DATABASE
Occurence 5524 - 313 Nyborg
(Object Id: 14965)
(Last updated: 24.02.2004)

Location
County: Troms Municipality: Målselv (5524)
Map 1:50000: Målselv (1433-2) Map 1:250000: Tromsø
Coordinate system: EU89-UTM Zone 34 (Coordinates NOT confirmed)
East: 397899 m. North: 7677499 m.
Longitude: 18.4244470 Latitude: 69.1882620
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Resource
Resource Type: Olivine Resource Subtype: Ultramafic (unspec.)

Importance
Raw material meaning: Not Assessed (reg. 18.02.2015)


Mineralization
Genesis: Form:
Main texture: Min. distribution:
Main grain size:
Strike/Dip: Direction:
Plunge:
Stratigraphic classification of host rock
Era: Period:
Province:
Geotec.unit:
Tectonic complex:
Igneous complex:
Group: Formation:

Bibliography:
From NGU's Reference Archive:
Karlsen, Tor Arne; Nilsson, Lars Petter , 2000
Talc deposits in Norway
;Norges geologiske undersøkelse;FAGRAPPORT;NGU-rapport; No.99.135;146 pages
Abstract:
Information about talc and soapstone deposits registered in NGU's different databases and various available literature have been collected and described in the present report. Around 400 deposits/occurrences are known, but the detail of the available information varies widely. By reading old field-books as well as old manuscripts, maps, etc. dating as far back as A.D.1758, quite a lot of data has been found. The result of the work shows that most described talc in Norway is of ultramafic origin and is associated with serpentinites. The most common mineral association is talc + breunnerite. Different talc-provinces can be defined from the registered and non-registered data, the most important being Nord-Gudbrandsdalen, Altermark and Stølsheimen. While Altermark and Stølsheimen have been investgated in some detail with respect to talc as an industrial mineral, the Nord-Gudbrandsdalen talc province has been investigated both for milling talc and for soapstone use as dimension stone. Deposits that are probably extensive, but have so far not been investigated in detail, include the Lesjehorrungane deposits in the Nord-Gudbrandsdalen region and the Raudfjellet deposit in Nord-Trøndelag. The fractionated metakomatiites (pale green talc-chlorite rocks) of the southern part of the Palaeo-proterozoic Karasjok Greenstone Belt in Finnmark, Northern Norway, possibly represents, by far, the largest accumulations of talc in Norway. These rocks are recently mapped, for the first time, but other critical information is, however, very scarce.

Zwaan, K.B.; Fareth, E.; Grogan, P.W. , 1998
Tromsø. Berggrunnskart Tromsø M 1:250 000; trykt i farger
;Norges geologiske undersøkelse;KART;1 kart pages
Abstract:
Beskrivelsen finnes på kartet.

References not to be found in NGU's Reference Archive.:
Landmark, K. 1974: Beskrivelse til de geologiske kartbladene Tromsø og Målselv. Et snitt gjennom fjellkjeden i Midt-Troms. Del II: A: Tekstbind, 259 sider med kart og tabeller. B: 103 fotos av bergarter. Tromsø Museums Skrifter, Vol XV.


The fact sheet was created on 05.05.2024

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