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MALMDATABASEN
Forekomstområde 805 - 001
(Sist oppdatert 12.apr.2016)

Navn på forekomstområde : Langesundsfjord
(Objekt Id : 0805,001,00,00)

Lokalisering
Fylke : Telemark (08) Kommune : Prosgrunn (0805)
Kart 1:50000: Porsgrunn (1713-2) Kart 1:250000: Skien
Markeringspunkt: Lengdegrad: 9.7527710 Breddegrad: 59.0245940
EU89-UTM Zone 32 (Koordinatene ER bekreftet)
X-koord: 543217 m. Y-koord: 6543033 m.

Materialtype
Hovedtype: Spesialmetaller (Nb,Ta,Be,Li,Sc,REE) Subtype: REE-metaller
Element(er): REE

Betydning
Offentlig: Ikke vurdert (reg. 06.05.2015)
Økonomisk: Ikke vurdert

Mineralisering
Æra: Paleozoikum Periode: Perm
Datering: 300 million år Metode:
Genese: Pegmatittdannelse Form:
Hovedtextur: Min. fordeling:
Kornstørrelse: Hovedomvandling:
Strøk/Fall: Retning:
Feltstupning:
Stratigrafisk klassifikasjon av vertsbergart
Æra: Periode:
Provins:
Geotek.enhet:
Tektonisk complex:
Intrusivt komplex:
Gruppe: Formasjon:

Mineralogi
Relasjon Mineral Mengde
Gangmineral Amfibol Hovedmineral (>10%)
Gangmineral Albitt Hovedmineral (>10%)
Gangmineral Ægirin Hovedmineral (>10%)
Gangmineral Nefelin Hovedmineral (>10%)
Malmmineral Eudialytt gruppen Aksessorisk mineral (<1%)
Malmmineral Hingganitt Aksessorisk mineral (<1%)
Malmmineral Loparitt Aksessorisk mineral (<1%)
Malmmineral Mosandritt Aksessorisk mineral (<1%)
Malmmineral Parisitt Aksessorisk mineral (<1%)
Malmmineral Gadolinitt Aksessorisk mineral (<1%)
Malmmineral Kainositt Aksessorisk mineral (<1%)
Malmmineral Monazitt Aksessorisk mineral (<1%)
Malmmineral Xenotim Aksessorisk mineral (<1%)
Malmmineral Chevkinitt Aksessorisk mineral (<1%)
Malmmineral Britholitt Aksessorisk mineral (<1%)
Malmmineral Bastnäsitt Aksessorisk mineral (<1%)
Malmmineral Allanitt Aksessorisk mineral (<1%)
Malmmineral Ancylitt Aksessorisk mineral (<1%)

Litologi:
Relasjon Bergart Opprinnelse
Vertsbergart Nepheline syenite Intrusiv
Opprinnelig bergart :Syenittpegmatitt

Opplysning(er) i fritekstformat
Fri tekst
The Langesundsfjord is part of the Permian Oslo Rift Province and one of the classic occurrences of peralkaline rocks. Some pegmatites are characterised by agpaite mineral associations. The location referenced here represents one of the observation points mentioned in literature; however, there are several occurrences spread over the Langesundsfjord and the area east of Langesundsfjord (see literature for details). Some of the pegmatites have been hydrothermally overprinted and are characterised by the presence of a variety of magmatic and hydrothermal minerals. Consequently, some of the minerals mentioned here as (potential) ore minerals are restricted to certain environments.

Litteraturfortegnelser:
Fra NGU's Referansearkiv.:
Andersen, T.; Erambert, M.; Larsen, A.O.; Selbekk, R. , 2010
Petrology of nepheline syenite pegmatites in the Oslo Rift, Norway: Zirconium silicate mineral assemblages as indicators of alkalinity and volatile fugacity in mildly agpaitic magma
;Oxford University Press;ARTIKKEL;Jounrnal of petrology; No.51 (11);2303-2325 sider

Brøgger, W.C. , 1890
Die Mineralien der Syenitpegmatitgänge der Südnorwegischen Augit- und Nephelinsyenite
;Verlag von Wilhelm Engelmann;BOK;Zeitschrift für Krystallographie und Mineralogie; No.16;4-658 sider

Schilling, J.; Wu, F.-Y.; McCammon, C.; Wenzel, T.; Marks, M.A.W.; Pfaff, K.; Jacob, D.E.; Markl, G. , 2011
The compositional variability of eudialyte-group minerals
;Mineralogical Society London;ARTIKKEL;Mineralogical magazine; No.75 (1);87-115 sider

Larsen, Alf Olav ; Dahlgren, Sven ; Berge, Svein Arne ; Andersen, Frode ; Larsen, Knut Edvard ; Burvald, Ingulv , 2010
The Langesundsfjord. History, geology, pegmatites, minerals
;Bode Verlag, Salzhemmendorf, Germany;BOK;239 s. sider
Abstrakt:

Larsen, Bjørn T.; Olaussen, Snorre; Sundvoll, Bjørn; Heeremans, Michel , 2008
The Permo-Carboniferous Oslo Rift through six stages and 65 million years
;IUGS;ARTIKKEL;Episodes; No.31 (1);52-58 sider
Abstrakt:
The Oslo Rift is the northernmost part of the Rotliegendes basin system in Europe. The rift was formed by lithospheric stretching north of the Tornquist fault system and is related tectonically and in time to the last phase of the Variscan orogeny. The main graben forming period in the Oslo Region began in Late Carboniferous, culminating some 20-30 Ma later with extensive volcanism and rifting, and later with uplift and emplacement of major batholiths. It ended with a final termination of intrusions in the Early Triassic, some 65 Ma after the tectonic and magmatic onset.

Neumann, Else-Ragnhild; Wilson, Marjorie; Heeremans, Michel; Spencer, Elizabeth Ann; Obst, Karsten; Timmerman, Martin J.; Kirstein, Linda , 2004
Carboniferous-Permian rifting and magmatism in southern Scandinavia and northern Germany: a review.
;Geological Society of London;ARTIKKEL;Geological Society Special Publication; No.223;11-40 sider

Larsen, A.O. , 1996
Rare earth minerals from the syenite pegmatites in the Oslo Region, Norway
;Chapman & Hall;ARTIKKEL;Mineralogical Society Series; No.7;151-166 sider


Faktaarket ble generert 25.11.2024

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