Fact Sheet for <b>Occurence 1824

					Norsk versjon
	THE INDUSTRIAL MINERAL DATABASE
	Occurence 1824 - 319 Remma
	(Object Id: 7680) (Last updated: 01.06.2010)

Location

County:

Nordland

Municipality:

Vefsn (1824)

Map 1:50000:

Fustvatnet (1926-4)

Map 1:250000:

Mosjøen

Coordinate system:

EU89-UTM Zone 33

(Coordinates NOT confirmed)

East:

420232 m.

North:

7303698 m.

Longitude:

13.2529360

Latitude:

65.8445950

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Resource

Resource Type:

Carbonates

Resource Subtype:

Dolomite

Importance

Raw material meaning:

Little Importance (reg. 18.02.2015)

Mineralization

Era: Paleozoic Period:

Genesis: Sedimentary/metamorphic Form: Layer

Main texture: Structureless Min. distribution: Massive (>50 % ore minerals)

Main grain size: Fine - medium grained (<1mm - 3 mm)

Strike/Dip: Direction:

Plunge:

Stratigraphic classification of host rock

Era: Paleozoic Period:

Province: Caledonides

Geotec.unit: Abisko Nappe Complex

Tectonic complex:

Igneous complex:

Group: Formation:

Information(s) in free text format

Free text

Ved Remmen på østsiden av Dolstadåsen. På sydsiden av Mosjøen eruptivfelt opptrer en kontaktmarmor. I kontakten mot eruptivmassivet kommer først en kontaktomvandlet skifersone på ca. 500 m med overgang til marmorsonene som stryker tilnærmet parallell med eruptivgrensen og mektigheten på draget er her ca. 100 m. I de 50 -60 m, som ligger nærmest eruptivmassivet, er marmoren middels til finkornet og hvit med noen grovere korn. Fargen er hvit med en svak grålig tone mens marmoren som ligger litt lengre bort fra eruptivkontakten er lyse grå og mer grovkrystallinsk. Denne kontaktmarmoren fra Remmen er delvis en dolomittmarmor Ref: Vogt NGU 22 s.257 og 258.

Bibliography:

From NGU's Reference Archive:

Vogt, Johan H.L. , 1897

Norsk marmor

;Norges geologiske undersøkelse;TIDSSKRIFTARTIKKEL;NGU; No.22;1-364 pages

Abstract:

Forkortet: Diese Arbeit zerfällt in vier Hauptabschnitte. 1. Über die Geologie des Marmors (S.4-18). 2. Über die wichtigsten Eigenschaften des Marmors, mit besonderer Rücksicht auf die norwegischen Marmorarten daneben über Betrieb usw der Brüche (S. 18-158). 3. Über die wichtigsten norwegischen Marmorfelder, hauptsächlich in der nord- norwegischen Glimmerschiefer-Marmor-Gruppe (S. 159-268); weiter in den Trondheim-schen Schiefern (S. 269-282): im Grundgebirge (S. 282-291); in der Bergen-schen Schiefern (S. 291-296), und Contactmarmor in dem Oslo-Gebiet (S. 296-303). 4. Zum Schluss eine wirthschaftliche über die Marmorproduction der Welt und über die Entwicklung der norwegischen Marmorindustrie.

Name of Sample point: amr13_10

(Object Id: 22294 319,00,01)

Location

County: Nordland Municipality: Vefsn (1824)

Map 1:50000: Fustvatnet (1926-4) Map 1:250000: Mosjøen

Coordinate system: EU89-UTM Zone 33

East: 420292 m. North: 7303756 m.

Longitude: 13.2542180 Latitude: 65.8451380

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Resource

Resource Type: Carbonates Resource Subtype: Dolomite

Fieldsamples

Sample No. Sample type Miscellanrous

AMR13_10 Bedrock

Sampler: Håvard Gautneb

Comment: Bergarten er en kalkstein som er ganske ren med et SiO2 innhold på -0.5% og et MgO innhold på 0.382%

No. of registrated element analyses = 1

No. of registrated oxide analyses = 1

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

Name of Sample point: amr14_10a

(Object Id: 22295 319,00,02)

Location

County: Nordland Municipality: Vefsn (1824)

Map 1:50000: Fustvatnet (1926-4) Map 1:250000: Mosjøen

Coordinate system: EU89-UTM Zone 33

East: 420299 m. North: 7303746 m.

Longitude: 13.2543780 Latitude: 65.8450420

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Resource

Resource Type: Carbonates Resource Subtype: Dolomite

Fieldsamples

Sample No. Sample type Miscellanrous

AMR14_10A Bedrock

Sampler: Håvard Gautneb

Comment: Bergarten er en kalkstein som er ganske ren med et SiO2 innhold på -0.5% og et MgO innhold på 0.443%

No. of registrated element analyses = 1

No. of registrated oxide analyses = 1

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

Analyse Results

from

Deposit Area 1824 - 319 Remma

Element analyses
( *=parts pr. million, #=parts pr.billion, Negative values means below detection limit value.)

Sample No. Sample Type Cu* Zn* Pb* Co* Ni* As* Cd*

AMR13_10 Bedrock -2 -4 -4 0 -2 -4 .0

AMR14_10A Bedrock -2 -4 -4 0 -2 -4 .0

------------------

Sample No. Ba* Mo* V* Cr* Mn* Fe% Sr* Y* Zr*

AMR13_10 5 -2.00 9 0 54 .01 1220.0 1.0 -4

AMR14_10A 3 -2.00 9 1 123 .30 621.0 3.0 -4

------------------

Sample No. La* Ce* B* Li* Be* Na* Mg* Al* Si*

AMR13_10 1.00 6.00 -20 -1 0 -400 2340 -40 -500

AMR14_10A 7.00 18.00 -20 2 0 -400 25800 308 511

------------------

Sample No. P* K * Ca* Sc* Ti*

AMR13_10 175 -200 ###### 0.00 5

AMR14_10A 142 528 ###### 1.00 20

Oxide analyses
( All values are in % )

Sample No. Sample Type SiO2 Al2O3 TiO2 Fe2O3 MnO MgO CaO

AMR13_10 Bedrock -0.50 0.04 -0.01 0.07 -0.01 0.38 55.90

AMR14_10A Bedrock -0.50 0.05 -0.01 0.05 -0.01 0.44 55.30

------------------

Sample No. Na2O K2O P2O5 Loss Sum

AMR13_10 -0.10 -0.01 0.03 43.00 99.00

AMR14_10A -0.10 -0.01 0.04 42.80 98.00

Era:	Paleozoic	Period:
Genesis:	Sedimentary/metamorphic	Form:	Layer
Main texture:	Structureless	Min. distribution:	Massive (>50 % ore minerals)

	Province:	Caledonides
	Geotec.unit:	Abisko Nappe Complex
	Tectonic complex:
	Igneous complex:

Sample No.	Sample Type	Cu*	Zn*	Pb*	Co*	Ni*	As*	Cd*
AMR13_10	Bedrock	-2	-4	-4	0	-2	-4	.0
AMR14_10A	Bedrock	-2	-4	-4	0	-2	-4	.0

Sample No.	Ba*	Mo*	V*	Cr*	Mn*	Fe%	Sr*	Y*	Zr*
AMR13_10	5	-2.00	9	0	54	.01	1220.0	1.0	-4
AMR14_10A	3	-2.00	9	1	123	.30	621.0	3.0	-4

Sample No.	La*	Ce*	B*	Li*	Be*	Na*	Mg*	Al*	Si*
AMR13_10	1.00	6.00	-20	-1	0	-400	2340	-40	-500
AMR14_10A	7.00	18.00	-20	2	0	-400	25800	308	511

Sample No.	P*	K *	Ca*	Sc*	Ti*
AMR13_10	175	-200	######	0.00	5
AMR14_10A	142	528	######	1.00	20

Sample No.	Sample Type	SiO2	Al2O3	TiO2	Fe2O3	MnO	MgO	CaO
AMR13_10	Bedrock	-0.50	0.04	-0.01	0.07	-0.01	0.38	55.90
AMR14_10A	Bedrock	-0.50	0.05	-0.01	0.05	-0.01	0.44	55.30

Sample No.	Na2O	K2O	P2O5	Loss	Sum
AMR13_10	-0.10	-0.01	0.03	43.00	99.00
AMR14_10A	-0.10	-0.01	0.04	42.80	98.00