Fact Sheet for <b>Occurence 0

					Norsk versjon
	THE ???? DATABASE
	Occurence 0 - 000 FEIL
	(Object Id: ) (Last updated: 19.03.2020)

Location

County:

Municipality:

Mangler ()

Map 1:50000:

Kongsberg (1714-2)

Map 1:250000:

Skien

Coordinate system:

UTM-Zone 33 - EUREF89/WGS84

East:

541600 m.

North:

6618150 m.

Longitude:

9.7390630

Latitude:

59.6978690

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Resource

	Resource Type:	Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn)	Resource Subtype:	Zinc
			Element(s):	Kis Zn Pb Cu

Importance

Raw material meaning:

Not Assessed (reg. 18.02.2015)

Resources and production

	Activity:	Pitting	Reserves:
	Operating method:		Historical production:

Mineralization

Era: Paleozoic Period: Permian

Genesis: Hydrothermal breccia Form: Irregular

Main texture: Vein network Min. distribution: Irregular (scattered)

Main grain size: Medium grained (1-3 mm) Main alteration:

Strike/Dip: 90 / 65 Direction:

Plunge:

Stratigraphic classification of host rock

Era: Proterozoic Period: Mesoproterozoic

Province: South Norwegian Basement Province

Geotec.unit: Kongsberg Complex

Tectonic complex:

Igneous complex:

Group: Formation:

Mineralogy

Relationship Mineral Amount

Gangue mineral Quartz Major mineral (>10%)

Gangue mineral Coal blende Subordinate mineral (1-10%)

Ore mineral Galena Major mineral (>10%)

Ore mineral Sphalerite Major mineral (>10%)

Ore mineral Pyrite Subordinate mineral (1-10%)

Ore mineral Chalcopyrite Subordinate mineral (1-10%)

Lithology:

Relationship Rock Origin

Host rock Felsic biotite gneiss Intrusive
Original rock :Granite

Metamorphic facies :Amphibolite

Structures

Location: Type: Orientation(360 gr.): Relation to min.:

Host rock Foliation Strike/Dip :15 / 90 Pre-mineralisation ;...Effect :None

Information(s) in free text format

Free text

Forekomsten består av en ca. 22 m lang dagskjæring med retning 95°. Skjæringen er gjenfylt og gjenvokst med en omkring 2 m høy vegg i nord og 1 m høy i sør. Den skjærer foliasjonen som har orientering 15°/90°, i felsisk, biotitt-førende gneis. Kvartsgangen er ikke synlig i skjæringen, men ulike faser med kvarts sees på tippen. Gangen er minst 30 cm bred og består hovedsakelig av melkehvit grovkornet kvarts med dels hulromsfylling. Blokker med mørk kvarts og kullblende finnes også. Sulfidmineralene forekommer i aggregater og disseminert i ulike faser av kvartsen. En ca. 45 cm bred kvartsgang er blottet i en 10 m lang, grunn grøft ca. 30 m vest for forekomsten (541535 6618086). Retningen på denne gangen er 90°/65°.

Fieldsamples

Sample No. Sample type Miscellanrous

BU0344.01 Bedrock

Sampler: J.S. Sandstad/...Stored: L›kken/...Size(kg): 2

Comment: Rik blyglans-kobberkis-sinkblende-pyritt i kvarts†re langs kontakten til pyritt- og kullblendef›rende kvarts

No. of registrated element analyses = 1

NB! All analyse values are shown at the end of the printout.:

Era:	Paleozoic	Period:	Permian
Genesis:	Hydrothermal breccia	Form:	Irregular
Main texture:	Vein network	Min. distribution:	Irregular (scattered)

	Province:	South Norwegian Basement Province
	Geotec.unit:	Kongsberg Complex
	Tectonic complex:
	Igneous complex:

Relationship	Mineral	Amount
Gangue mineral	Quartz	Major mineral (>10%)
Gangue mineral	Coal blende	Subordinate mineral (1-10%)
Ore mineral	Galena	Major mineral (>10%)
Ore mineral	Sphalerite	Major mineral (>10%)
Ore mineral	Pyrite	Subordinate mineral (1-10%)
Ore mineral	Chalcopyrite	Subordinate mineral (1-10%)

Relationship	Rock	Origin
Host rock	Felsic biotite gneiss	Intrusive Original rock :Granite
		Metamorphic facies :Amphibolite

	Location:	Type:	Orientation(360 gr.):	Relation to min.:
	Host rock	Foliation	Strike/Dip :15 / 90	Pre-mineralisation ;...Effect :None