Faktarka for <b>Registrering 5524

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	INDUSTRIMINERALDATABASEN
	Registrering 5524 - 313 Nyborg
	(Objekt Id: 14965) (Sist oppdatert: 24.02.2004)

Lokalisering

Fylke:

Troms

Kommune:

Målselv (5524)

Kart 1:50000:

Målselv (1433-2)

Kart 1:250000:

Tromsø

Koordinatsystem:

EU89-UTM Zone 34

(Koordinatene IKKE bekreftet)

Øst:

397899 m.

Nord:

7677499 m.

Lengdegrad:

18.4244470

Breddegrad:

69.1882620

Kartvisning

Ressurs

Ressurstype:

Olivin

Ressursundertype:

Ultramafitt (uspes.)

Betydning

Råstoffbetydning:

Ikke vurdert (reg. 18.02.2015)

Mineralisering

Genese: Form:

Hovedtekstur: Min. fordeling:

Kornstørrelse:

Strøk/Fall: Retning:

Feltstupning:

Stratigrafisk klassifikasjon av vertsbergart

Æra: Periode:

Provins:

Geotek.enhet:

Tektonisk complex:

Intrusivt komplex:

Gruppe: Formasjon:

Litteraturfortegnelser:

Fra NGU's Referansearkiv.:

Karlsen, Tor Arne; Nilsson, Lars Petter , 2000

Talc deposits in Norway

;Norges geologiske undersøkelse;FAGRAPPORT;NGU-rapport; No.99.135;146 sider

Abstrakt:

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 sider

Abstrakt:

Beskrivelsen finnes på kartet.

Referanser som ikke finnes i NGU's Referansearkiv.:

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.

	Provins:
	Geotek.enhet:
	Tektonisk complex:
	Intrusivt komplex: