Fact Sheet for <b>Occurence 3120

					Norsk versjon
	THE INDUSTRIAL MINERAL DATABASE
	Occurence 3120 - 383 Skrukka
	(Object Id: 8920) (Last updated: 21.11.2006)

Location

County:

Østfold

Municipality:

Rakkestad (3120)

Map 1:50000:

Sarpsborg (1913-1)

Map 1:250000:

Oslo

Coordinate system:

EU89-UTM Zone 32

(Coordinates NOT confirmed)

East:

636918 m.

North:

6595792 m.

Longitude:

11.4171120

Latitude:

59.4782170

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Resource

Resource Type:

Mica minerals

Resource Subtype:

Pegmatitic muscovite

Importance

Raw material meaning:

Little Importance (reg. 18.02.2015)

Resources and production

	Activity:	Mining	Reserves:
	Operating method:	Open pit mining	Historical production:

Operations

From - To Activity Comments

1917 - 1918 Regular production Company/Institution :Smaalenes Glimmerkompani

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:

Information(s) in free text format

Free text

Bruddet ligger ca. 200 meter syd for Skrukka, Syd for Holtet. Pegmatitten skjærer en massiv gabbro og er på det bredeste ca. 4 meter. Strøket er nordøstlig. Forekomsten har hovedsaklig vært drevet som en glimmergruve, men det er også tatt ut litt gråhvit kalifeltspat. Siste gang forekomsten var i drift var i perioden 1917-1918.

Bibliography:

From NGU's Reference Archive:

Broch, Olaf Anton , 1934

Feltspat IV. Forekomster i Akershus og Østfold øst for Glomma.

;Norges geologiske undersøkelse;TIDSSKRIFTARTIKKEL;NGU; No.141;1-119 pages

Abstract:

In this publication, which is a sequel to Feltspat II and III by Olaf Andersen and Tom F.W. Barth, brief and exoteric descriptions and some information on production and history are given of about 180 individual feldspar, quartz, and mica deposits, all of them situated east of the river Glomma in south-eastern Norway. Particulars of purely geological or mineralogical interest are few; most of them are given as footnotes or in the preface, but the minerals of each deposit, exceot quartz, feldspar and mica, are listed. The deposits are cross cutting pegmatite dikes, with a northeastern strike and a steep dip. The dikes exhibit a marked zoning; moreover, they are remarkably free from rare minerals, the occurrences of which seems to be restricted almost entirely to the dikes near the Idefjord (Bohus) granite.

	From - To	Activity	Comments
	1917 - 1918	Regular production	Company/Institution :Smaalenes Glimmerkompani

	Genesis:		Form:
	Main texture:		Min. distribution:

	Province:
	Geotec.unit:
	Tectonic complex:
	Igneous complex: