Fact Sheet for <b>Occurence 0

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	Occurence 0 - 000 FEIL
	(Object Id: ) (Last updated: 02.02.2004)

Location

County:

Municipality:

Mangler ()

Map 1:50000:

Seiland (1835-1)

Map 1:250000:

Hammerfest

Coordinate system:

UTM-Zone 33 - EUREF89/WGS84

(Coordinates NOT confirmed)

East:

587100 m.

North:

7801600 m.

Longitude:

23.3159090

Latitude:

70.3036340

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Resource

Resource Type:

Olivine

Resource Subtype:

Olivine

Importance

Raw material meaning:

Not Assessed (reg. 18.02.2015)

Mineralization

Genesis: Form:

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Stratigraphic classification of host rock

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Mineralogy

Mineral Amount

Olivine Major mineral (>10%)

Information(s) in free text format

Free text

Lokaliteten er opprinnelig plottet av A.O.Poulsen på hans 1:100.000 kart Komagfjord. På Vargsund-siden av Habuvarri opptrer her en olivin-pyroksenitt med peridotittpartier. Maksimum 80% olivin angies i litteraturen.

Bibliography:

From NGU's Reference Archive:

Bennett, M.C.; Emblin, S.R.; Robins, B.; Yeo, W.J.A. , 1986

High-temperature ultramafic complexes in the North Norwegian Caledonides: I - Regional setting and field relationships.

;Norges geologiske undersøkelse;TIDSSKRIFTARTIKKEL;NGU Bulletin; No.405;1-40 pages

Abstract:

Forkortet. Four major (25-100 km²) ultramafic complexes were developed in the Sørøy Nappe during the second phase of Finnmarkian deformation in the North Norwegian Caledonides. They were emplaced into layered mafic intrusions and show broadly similar emplacement histories and petrographic variations suggesting a related petrogenesis. The Nordre Bumannsfjord, Melkvann and Kvafjord group of ultramafic complexes developed in part by emplacement of both replacive and dilational ne-normative ultramafic sheets and dykes which progressively fragmented the layered olivine gabbro envelope. The Reinfjord ultramafic complex contains pronounced, subhorizontal modal layering and evidence of at least 3 major magmatic events. The intrusive sequences and petrographic variations represented in the complexes suggest the succesive emplacement of mantle-derived magmas with a diminishing number of liquidus phases, accompanied by in situ liquid-crystal fractionation, subsidiary hybridization and metasomatism.

Oosterom, M.G. , 1963

The ultramafites and layered gabbro sequences in the granulite facies rocks on Stjernøy.

;AVHANDLING;296 s. pages

Abstract:

På Stjernøy, Seiland og på fastlandet ved Øksfjord og Bergsfjord finne peridotitt, pyroksenitt og lagdelt gabbro innenfor et kompleks av høymetamorfte gabbro gneisser. Den lagdelte gabbro er i alminnelighet konkordant med parallellstrukturen i de omliggende gneiser, men viser lokalt uregelmessigheter (se kart i lommen bak i boken). Også hornblenditt, karbonatitt og nefelinsyenitt forekommer, de er sannsynligvis dannet ved metasomatiske prosesser. (Forkortet)

References not to be found in NGU's Reference Archive.:

Barth, T.F.W. 1927: Die pegmatitgänge der kaledonischen Intrusivgesteine im Seiland-Gebiete. .....Vid.-Akad.Skr.Mat.-Nat. Kl. 1927, No 8, 123 s.

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