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	THE ???? DATABASE
	Occurence 0 - 000 FEIL
	(Object Id: ) (Last updated: 03.04.2002)

Operations

	From - To	Activity	Comments
	1974 - 1974	Sampling	Company/Institution :A/S Sulfidmalm
	1998 - 1998	Sampling	Company/Institution :NGU

Mineralization

	Era:	Proterozoic	Period:	Neoproterozoic
	Genesis:	Volcex	Form:	Lens
	Main texture:	Banded	Min. distribution:	Semi-massive (20-50 % ore minerals)

Main grain size:

Fine grained (< 1 mm)

Main alteration:

No country rock alteration

	Strike/Dip:	18 / 15	Direction:
			Plunge:

Stratigraphic classification of host rock

Era:

Proterozoic

Period:

Neoproterozoic

	Province:	Caledonides
	Geotec.unit:	Trondheim Nappe Complex
	Tectonic complex:	Gula Nappe
	Igneous complex:

Group:

Gula

Formation:

Mineralogy

	Relationship	Mineral	Amount
	Gangue mineral	Quartz	Major mineral (>10%)
	Gangue mineral	Garnet	Major mineral (>10%)
	Gangue mineral	Amphibole	Major mineral (>10%)
	Ore mineral	Pyrrhotite	Major mineral (>10%)
	Ore mineral	Arsenopyrite	Subordinate mineral (1-10%)
	Ore mineral	Magnetite	Accessory mineral (<1%)
	Ore mineral	Chalcopyrite	Accessory mineral (<1%)

Lithology:

	Relationship	Rock	Origin
	Wall rock	Amphibolite	Extrusive Original rock :Basalt
			Metamorphic facies :Amphibolite
	Wall rock	Garnet mica schist	Sedimentary Original rock :Greywacke
			Metamorphic facies :Amphibolite

Structures

	Location:	Type:	Orientation(360 gr.):	Relation to min.:
	Host rock	Mineral banding	Strike/Dip :18 / 15	Syn-mineralisation ;...Effect :Controls
	Wall rock	Foliation	Strike/Dip :28 / 20	Post-mineralisation ;...Effect :Modifies

Information(s) in free text format

Free text

Sæterfjellet ligger 4 km nord for Kviknegruvene på nordsida av Ya. Flere mindre skjerp som ligger i nordøstskråningen av fjellet. Sæterfjellet kisfelt som er omtalt i eldre rapporter (Berg 1917), inkluderer trolig også i tillegg forekomstene Russu (HE0144) og Svartsjøen (HE0145) og ble fram mot 1. verdenskrig undersøkt av bergasessor Spinzig. Hovedforekomsten er et skjerp som er skutt i nordøstskråningen av en mindre rygg, ca. 600 m nordøst for toppen av Sæterfjellet. Det har en 3 m høy skjæring i vest og tipp på 30 m3. Malmsonen er ca. 2.5 m mektig og i likhet med vertsbergartene kraftig rustfarget. Under malmsonen ligger finkornet amfibolitt med foliasjon 28°/20° mens granatrik biotittskifer følger over malmen. Malmen kan best studeres på tippen. Semi-massiv magnetkis dominerer og aksessorisk opptrer kobberkis og arsenkis. Malmen er dels båndet med orientering 18°/15, og viktigste gangmineralene er kvarts, granat og amfibol. Området nordøstover mot de mindre skjerpene er overdekket av løsmasser.

Photo(s) from the Deposit area:

Photo no. 1 showing Sæterfjell hovedskjerp"

Bibliography:

From NGU's Reference Archive:

Nilsen, Odd , 1978

	Caledonian sulphide deposits and minor iron-formations from the southern Trondheim region, Norway.

;Norges geologiske undersøkelse;TIDSSKRIFTARTIKKEL;NGU; No.340;35-85 + k pages

Abstract:

Within the southern and central parts of the Trondheim region of the Norwegian Caledonides a great number of small, stratabound cupriferous pyrite deposits are confined to mafic metavolcanics of the Gula, Støren and Fundsjø Groups of the Lower Palaeozoic succession. The deposits occuring within, or in close contact with the metavolcanics are characterized by their association with minor manganiferous oxide/silicate iron-formations - better known as "vasskis" ore type - within the metamorphic low-grade areas. The iron-fprmations of the metamorphic higher grade terrains on the other hand, which are extensively developed within the Gula Group, are mostly of a pyrrhotitic sulphide/silicate type and sulphurization processes are thought to have played an important role during the metamorphism. The pyrite deposits occurring adjacent to the metavolcanics bear no relationship to the iron-formations. They are embedded in pelitic, often carbonaceous assemblages (Gula Group) or within tuffitic members of the volcanogene Støren Group, and they are thought to represent re-sedimented (reworked) deposits. The pyrite deposits display varying degree of metamorphic reconstitution and a tectonic control has apparently determined their disc- or ruler-shaped morphology.

Berg, P. J. , 1917

	Sæterfjeldets kisfelt.

;Norges geologiske undersøkelse;FAGRAPPORT;Bergarkivet; No.BA 1772;1 pages

	Abstract:
	Rapporten beskriver følgende forekomster: - Sæterfjellets kisfelt som opptrer som en rekke ganger med stor regelmessighet og med mektigheter fra en til ti meter. Malmmineraliseringen er kobberholdig svovelkis. - Sandfjellets kisfelt, forekomstene er lite undersøkt. - Løken, Estermoen og Orkelbogen er et ca 10 km langt felt med betydelige mektigheter.

Boe, dr. , 1910?

	Seterfjellet, Tynset, Hedmark.

;Norges geologiske undersøkelse;FAGRAPPORT;Bergarkivet; No.BA 2146;4 pages

	Abstract:
	Rapporten er et kopi av håndgivelsesdokument og omhandler Sæterfjellets kobber og kisforekomster. Det blir gitt en nøye spesifikasjon over hva som inngår i kontrakten.

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

Sivertsen, R. 1975: Geological, geophysical and diamond drilling investigations in the Kvikne area 1974. Project 905.20. Bergvesenet rapport nr. BV 1014, 21s.

Fieldsamples

	Sample No.	Sample type	Miscellanrous
	HE0142.01	Dump	Sampler: J.S. Sandstad/...Stored: Løkken Comment: Semi-massiv, finkornet magnetkis+kobberkis+arsenkis, kobberkis-årer, kvarts-granat rik matriks No. of registrated element analyses = 1
	HE0142.02	Dump	Sampler: J.S. Sandstad/...Stored: Løkken Comment: Massiv, finkornet magnetkis+kobberkis, kobberkis langs små kvartsboller No. of registrated element analyses = 1
	HE0142.03	Dump	Sampler: J.S. Sandstad/...Stored: Løkken Comment: Semi-massiv magnetkis+arsenkis+kobberkis i kvartsrik matriks No. of registrated element analyses = 1

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

Name of Locality: Sæterfjell II

(Object Id: 10196 38,01,00)

Location

County:

Municipality:

Mangler ()

Map 1:50000:

Kvikne (1620-3)

Map 1:250000:

Røros

Coordinate system:

UTM-Zone 33 - EUREF89/WGS84

East:

574550 m.

North:

6940780 m.

Longitude:

10.4530970

Latitude:

62.5906210

Show on map

Resource

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

Resources and production

	Activity:	Pitting	Reserves:
	Operating method:		Historical production:

Operations

	From - To	Activity	Comments
	1998 - 1998	Sampling	Company/Institution :NGU

Mineralogy

	Relationship	Mineral	Amount
	Gangue mineral	Plagioclase	Major mineral (>10%)
	Gangue mineral	Amphibole	Major mineral (>10%)
	Ore mineral	Pyrrhotite	Major mineral (>10%)
	Ore mineral	Pyrite	Subordinate mineral (1-10%)
	Ore mineral	Chalcopyrite	Accessory mineral (<1%)

Lithology:

	Relationship	Rock	Origin
	Host rock	Amphibolite	Extrusive Original rock :Basalt
			Metamorphic facies :Amphibolite
	Wall rock	Quartzite	Sedimentary Original rock :Exhalite
			Metamorphic facies :Amphibolite

Information(s) in free text format

Free text

En nordøst-sørvest orientert, 10 m lang og opptil 1 m dyp gjenrast røskegrøft går gjennom en mindre rygg. Bergartene er kraftig rustforvita, men middelskornet kvartsitt og amfibolitt gjenkjennes. Amfibolitten fører disseminasjon og årer med hovedsakelig magnetkis og mindre mengder pyritt og kobberkis (prøve -04).

Bibliography:

From NGU's Reference Archive:

Berg, P. J. , 1917

	Sæterfjeldets kisfelt.

;Norges geologiske undersøkelse;FAGRAPPORT;Bergarkivet; No.BA 1772;1 pages

	Abstract:
	Rapporten beskriver følgende forekomster: - Sæterfjellets kisfelt som opptrer som en rekke ganger med stor regelmessighet og med mektigheter fra en til ti meter. Malmmineraliseringen er kobberholdig svovelkis. - Sandfjellets kisfelt, forekomstene er lite undersøkt. - Løken, Estermoen og Orkelbogen er et ca 10 km langt felt med betydelige mektigheter.

Nilsen, Odd , 1978

	Caledonian sulphide deposits and minor iron-formations from the southern Trondheim region, Norway.

;Norges geologiske undersøkelse;TIDSSKRIFTARTIKKEL;NGU; No.340;35-85 + k pages

Abstract:

Within the southern and central parts of the Trondheim region of the Norwegian Caledonides a great number of small, stratabound cupriferous pyrite deposits are confined to mafic metavolcanics of the Gula, Støren and Fundsjø Groups of the Lower Palaeozoic succession. The deposits occuring within, or in close contact with the metavolcanics are characterized by their association with minor manganiferous oxide/silicate iron-formations - better known as "vasskis" ore type - within the metamorphic low-grade areas. The iron-fprmations of the metamorphic higher grade terrains on the other hand, which are extensively developed within the Gula Group, are mostly of a pyrrhotitic sulphide/silicate type and sulphurization processes are thought to have played an important role during the metamorphism. The pyrite deposits occurring adjacent to the metavolcanics bear no relationship to the iron-formations. They are embedded in pelitic, often carbonaceous assemblages (Gula Group) or within tuffitic members of the volcanogene Støren Group, and they are thought to represent re-sedimented (reworked) deposits. The pyrite deposits display varying degree of metamorphic reconstitution and a tectonic control has apparently determined their disc- or ruler-shaped morphology.

Fieldsamples

	Sample No.	Sample type	Miscellanrous
	HE0142.04	Bedrock	Sampler: J.S. Sandstad/...Stored: Løkken Comment: Grovkornet disseminasjon/aggregater av magnetkis+pyritt i middelskornet amfibolitt No. of registrated element analyses = 1

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

Name of Locality: Sæterfjell III

(Object Id: 10197 38,02,00)

Location

County:

Municipality:

Mangler ()

Map 1:50000:

Kvikne (1620-3)

Map 1:250000:

Røros

Coordinate system:

UTM-Zone 33 - EUREF89/WGS84

East:

574480 m.

North:

6940730 m.

Longitude:

10.4517120

Latitude:

62.5901860

Show on map

Resource

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

Resources and production

	Activity:	Pitting	Reserves:
	Operating method:		Historical production:

Operations

	From - To	Activity	Comments
	1998 - 1998	Sampling	Company/Institution :NGU

Mineralogy

	Relationship	Mineral	Amount
	Gangue mineral	Quartz	Major mineral (>10%)
	Gangue mineral	Garnet	Subordinate mineral (1-10%)
	Ore mineral	Pyrrhotite	Major mineral (>10%)
	Ore mineral	Magnetite	Subordinate mineral (1-10%)
	Ore mineral	Chalcopyrite	Accessory mineral (<1%)

Lithology:

	Relationship	Rock	Origin
	Host rock	Dark quartzite	Sedimentary Original rock :Exhalite
			Metamorphic facies :Amphibolite
	Wall rock	Amphibolite	Extrusive Original rock :Basalt
			Metamorphic facies :Amphibolite

Information(s) in free text format

Free text

Skjerpet ligger 80 m sørvest for Sæterfjell II på nordsida av en markert rygg i terrenget hvor det er skutt ut en 2 x 3 m vannfyllt grop. Ryggen består i hovedsak av finkornet, mørk kvartsitt med varierende magnetitt disseminasjon (prøve -05). Den er opptil 1.5 m mektig og fører også enkelte sulfidårer og er sterkt rustfarget ved gropa i nord. I den 10 m3 store tippen finnes mange blokker med massiv, middelskornet magnetkis (prøve .06) og finkornet amfibolitt. Tippmateriale er ikke blottet i fast fjell.

Bibliography:

From NGU's Reference Archive:

Berg, P. J. , 1917

	Sæterfjeldets kisfelt.

;Norges geologiske undersøkelse;FAGRAPPORT;Bergarkivet; No.BA 1772;1 pages

	Abstract:
	Rapporten beskriver følgende forekomster: - Sæterfjellets kisfelt som opptrer som en rekke ganger med stor regelmessighet og med mektigheter fra en til ti meter. Malmmineraliseringen er kobberholdig svovelkis. - Sandfjellets kisfelt, forekomstene er lite undersøkt. - Løken, Estermoen og Orkelbogen er et ca 10 km langt felt med betydelige mektigheter.

Nilsen, Odd , 1978

	Caledonian sulphide deposits and minor iron-formations from the southern Trondheim region, Norway.

;Norges geologiske undersøkelse;TIDSSKRIFTARTIKKEL;NGU; No.340;35-85 + k pages

Abstract:

Within the southern and central parts of the Trondheim region of the Norwegian Caledonides a great number of small, stratabound cupriferous pyrite deposits are confined to mafic metavolcanics of the Gula, Støren and Fundsjø Groups of the Lower Palaeozoic succession. The deposits occuring within, or in close contact with the metavolcanics are characterized by their association with minor manganiferous oxide/silicate iron-formations - better known as "vasskis" ore type - within the metamorphic low-grade areas. The iron-fprmations of the metamorphic higher grade terrains on the other hand, which are extensively developed within the Gula Group, are mostly of a pyrrhotitic sulphide/silicate type and sulphurization processes are thought to have played an important role during the metamorphism. The pyrite deposits occurring adjacent to the metavolcanics bear no relationship to the iron-formations. They are embedded in pelitic, often carbonaceous assemblages (Gula Group) or within tuffitic members of the volcanogene Støren Group, and they are thought to represent re-sedimented (reworked) deposits. The pyrite deposits display varying degree of metamorphic reconstitution and a tectonic control has apparently determined their disc- or ruler-shaped morphology.

Fieldsamples

	Sample No.	Sample type	Miscellanrous
	HE0142.05	Bedrock	Sampler: J.S. Sandstad/...Stored: Løkken Comment: Svak magnetitt disseminasjon i finkornet grå kvartsitt No. of registrated element analyses = 1
	HE0142.06	Dump	Sampler: J.S. Sandstad/...Stored: Løkken Comment: Massiv, middelskornet magnetkis, kvart-granat matriks No. of registrated element analyses = 1

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

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The fact sheet was created on 29.04.2024

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