Faktarka for <b>Registrering 5605 - 307 Galsaluobbal</b>

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	INDUSTRIMINERALDATABASEN
	Registrering 5605 - 307 Galsaluobbal
	(Objekt Id: 14942) (Sist oppdatert: 24.02.2004)

Lokalisering

Fylke:

Finnmark

Kommune:

Sør-Varanger (5605)

Kart 1:50000:

Neiden (2334-2)

Kart 1:250000:

Kirkenes

Koordinatsystem:

EU89-UTM Zone 36

(Koordinatene IKKE bekreftet)

Øst:

355197 m.

Nord:

7742146 m.

Lengdegrad:

29.2498140

Breddegrad:

69.7473540

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.:

Nilsson, L.P.; Iversen, E. , 1991

Neiden. Berggrunnskart; Neiden; 23342; 1:50 000; sort/hvitt;

;Norges geologiske undersøkelse;KART

Iversen, E.; Nilsson, L.P. , 1991

Høybuktmoen. Berggrunnskart; Høybuktmoen; 24343; 1:50 000; sort/hvitt;

;Norges geologiske undersøkelse;KART

Wiik, Viggo H. , 1966

Petrological studies of the Neiden granite complex.

;Norges geologiske undersøkelse;TIDSSKRIFTARTIKKEL;NGU; No.237;1-99 sider

Abstrakt:

The Neiden granite complex fits well into Raguin's group of "anatectic granites with suites of migmatites". In this area, supracrustals of the Bjørnevatn group have, together with their gneissgranitic basement, been subjected to ultrametamorphism. The resulting rocks are classified as gneissgranite, granodiorite and quartz monzonite, these granitoids being separated from the surrounding gneiss by a zone of transition migmatites. Certain features of this zone are best explained by assuming partial anatexis. The totality of observed phenomena can not be accounted for by any purely magmatic metasomatic hypothesis alone, and the proposed petrogenetic model is intended as a working hypothesis rather than a final conclusion. In addition to the conventional methods, studies of the geographical areal variation of Fe, K and Na content of the rock and radioactivity in the field were performed for one particular sub-area. The perhaps most interesting result of this variation study is the strong indication that granodiorite did form by some - practically in situ - transformation of rocks of the Bjørnevatn group. Trend surface analysis has been applied to these quantitative data, adding to the gradually accumulating experience with this method in geology.

Siedlecka, Anna; Nordgulen, Øystein , 1996

Kirkenes. Berggrunnsgeologisk kart Kirkenes M 1:250 000; trykt i farger

;Norges geologiske undersøkelse;KART;1 kart sider

Abstrakt:

Beskrivelsen finnes på kartet.

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