Norsk versjon | |||||
THE ORE DATABASE | |||||
Deposit Area 1833 - 066 | |||||
(Last updated 14.feb.2017) |
Name of Deposit Area : Raudsandhaugen |
(Object Id : 1833,066,00,00) |
The deposit area belongs to the Province : Mofjellet sink-bly |
Drill Cores from the Deposit Area: See Borehole Area Raudsandhaugen |
Location |
County : | Nordland (18) | Municipality : | Rana (1833) |
Map 1:50000: | Storforshei (2027-4) | Map 1:250000: | Mo i Rana |
Marking point: | Longitude: | 14.5848180 | Latitude: | 66.2904430 |
EU89-UTM Zone 33 | (Coordinates IS confirmed) |
X-coord: | 481370 m. | Y-coord: | 7352346 m. |
|
Commodity |
Main Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Sub Type: | Zinc | |
Element(s): | Kis Zn Pb |
Production |
Activity: | Pitting | Reserves: | ||
Prod. method: | Production: | ,05 thousand tons | ||
Prod. status: | Volume of dump: | 85 m3 |
Importance |
Public: | Not Assessed (reg. 18.02.2015) |
Economical: | Not classified/evaluated |
Products |
Element/product | Crude ore grade or quality | |
CU | .1 % | |
KIS | 40 % | |
ZN | 4 % |
Operations |
From - To | Activity | Comments | |
1917 - 1917 | Pitting | ||
1976 - 1976 | Geophysics | ||
1981 - 1981 | Geology | ||
1984 - 1984 | Geophysics | ||
1984 - 1984 | Core drilling | Company/Institution :BNN A/S | |
2007 - 2007 | Geophysics | Company/Institution :GEXCO Norge AS | |
TEM, magnetometry | |||
2008 - 2009 | Geology | Company/Institution :NGU | |
Mapping, sampling |
Mineralization |
Era: | Proterozoic | Period: | Neoproterozoic | |
Dating: | Method: | |||
Genesis: | Volcex | Form: | Lens | |
Main texture: | Porphyroblastic | Min. distribution: | Semi-massive (20-50 % ore minerals) |
Main grain size: | Medium grained (1-3 mm) | Main alteration: |
Strike/Dip: | 265 / 85 | Direction: | 280 | |
Plunge: | 45 |
Stratigraphic classification of host rock |
Era: | Proterozoic | Period: | Neoproterozoic |
Province: | Caledonides | |
Geotec.unit: | Rødingsfjell Nappe Complex | |
Tectonic complex: | Uppermost Allochthon | |
Igneous complex: |
Group: | Mofjell Group | Formation: |
Mineralogy |
Relationship | Mineral | Amount | |
Gangue mineral | Quartz | Major mineral (>10%) | |
Gangue mineral | Muscovite | Subordinate mineral (1-10%) | |
Gangue mineral | Biotite | Subordinate mineral (1-10%) | |
Gangue mineral | Plagioclase | Subordinate mineral (1-10%) | |
Gangue mineral | Staurolite | Subordinate mineral (1-10%) | |
Gangue mineral | Epidote | Accessory mineral (<1%) | |
Gangue mineral | Garnet | Accessory mineral (<1%) | |
Gangue mineral | Gahnite | Accessory mineral (<1%) | |
Ore mineral | Pyrite | Major mineral (>10%) | |
Ore mineral | Sphalerite | Major mineral (>10%) | |
Ore mineral | Pyrrhotite | Subordinate mineral (1-10%) | |
Ore mineral | Galena | Accessory mineral (<1%) | |
Ore mineral | Chalcopyrite | Accessory mineral (<1%) |
Lithology: |
Relationship | Rock | Origin | |
Host rock | Muscovite gneiss | Extrusive | |
Metamorphic facies :Amphibolite | |||
Wall rock | Amphibolite | Extrusive Original rock :Basalt |
|
Metamorphic facies :Amphibolite | |||
Wall rock | Qz-fsp gneiss | Extrusive | |
Metamorphic facies :Amphibolite |
Structures |
Location: | Type: | Orientation(360 gr.): | Relation to min.: | |
Host rock | Foliation | Strike/Dip :265 / 85 | Post-mineralisation ;...Effect :Controls | |
Host rock | Fold axis | Strike/Dip :280 / 45 | Post-mineralisation ;...Effect :Modifies |
Information(s) in free text format |
Free text |
The Raudsandhaugtjern, Raudsandhaugen and Raudfjell East mineralizations to the east of Raudvatnet consist of more than 20 small prospects and showings over a strike length of more than 3 km, all situated in the same muscovite gneiss layer. Pyrite is the dominant sulfide, occurring in rich impregnations to thin semi-massive stripes in quartz-sericite schist. Locally the mineralizations reach thicknesses of 3-4 m, but approx. 1 m is more common. Generally the contents of base metals are very low, with Cu+Zn+Pb contents of 0.05-2.2 %. In the main prospects the content of zinc is 1-2 %, and is found as sphalerite, as zinc spinel (gahnite) in 1.2 mm bluish-green crystals and as zinc staurolite in up to cm-sized orange prismatic crystals. The mineralogy observed in thin sections confirms that the mineralizations are dominated by pyrite, while sphalerite and locally chalcopyrite and/or galena occur in accessory amounts. Quartz, muscovite, biotite and plagioclase are the main gangue minerals. |
Bibliography: |
From NGU's Reference Archive: |
Bjerkgård, Terje ; Marker, Mogens ; Slagstad, Trond ; Solli, Arne , 2008 |
Mofjell-prosjektet. Statusrapport 2008 |
;Norges geologiske undersøkelse;RAPPORT;NGU-rapport; No.2008.088;25 s. pages |
Abstract: | |
Rapporten gir en status for Mofjellprosjektet, et 4-årig samarbeidsprosjekt mellom GEXCO Norge AS og NGU. Prosjektområdet er øst og sør for Mo i Rana, et område som kan inneholde økonomiske sulfidforekomster med Cu, Zn, Pb, Ag og Au. Målet er å få fram dette potensialet gjennom å kartlegge berggrunnen, de kjente og delvis drevne sulfidforekomstene og andre mineraliseringer i området. Berggrunnskartleggingen i 2008 har fokusert på den østlige delen av området, som omfatter fortsettelsen av Plurdalgruppen sørover og relasjonen til bergartsgrupper i øst. Dette innbefatter den viktige tidlig Kaledonske skyvestrukturen som kalles Langfjellsonen, som kan representere et malmgeologisk provinsielt skille, med jernmalmene i nord og sulfidforekomstene i sør. Under feltarbeidet ble det systematisk innsamlet 95 bergartsprøver til geokjemi, geokronologi og petrologi for å undersøke bergartenes dannelse som bakgrunn for relasjonen til malmgenese. Malmgeologiarbeidet har i 2008 fokusert på å skaffe oversikt over sulfidforekomster i Mofjellgruppen og en rekke nøkkelforekomster i de forskjellige mineraliserte sonene er kartlagt og prøvetatt. I tillegg har GEXCO innsamlet mange prøver, dels i form av håndstykkeprøver og dels i form av boring med packsack utstyr. Sammen med resultater fra GEXCOs diamantboringer viser arbeidet så langt at en rekke forekomster og soner i området kan være av økonomisk interesse og bør følges opp videre. De mest interessante områdene og forekomstene i Mofjellgruppen som peker seg ut så langt i tillegg til forekomstene i Mofjellet og Sølvberget er Hellerfjellet, Hesjelia-Hammertjønna, Heramb-Bertelberget og Småvatnan. Mer arbeid med dataene, blant annet sammenholdt med data fra tidligere prospekteringsaktivitet i området, er nødvendig for å komme nærmere inn på potensialet i både de ovenfor nevnte forekomstene og andre i området. |
Bjerkgård, Terje; Marker, Mogens; Slagstad, Trond; Solli, Arne , 2013 |
The Mofjell project: summary and conclusions |
;Norges geologiske undersøkelse;RAPPORT;NGU-rapport; No.2013.048;87 pages |
Abstract: | |
The Mofjell project commenced in 2008 as a cooperation between GEXCO Norge AS, the county administration of Nordland and NGU. As GEXCO faced financial difficulties the external funding ended in 2009. The project area included Mofjellet and the eastern part of Plurdalen, an area with a large potential for economic sulfide deposits with Zn, Cu, Pb, Ag and Au. NGU has focused on establishing the geological setting of the Mofjell Group and its relation to ore formation. Another very important goal has been to assess the potential for economic ore deposits in the area, including enrichment of precious metals. On the basis of lithological observations and geochemistry, the Mofjell Group consists of a largely bimodal volcanic-sedimentary assemblage formed in an island-arc to back-arc setting. The data also show that the proportion of felsic volcanic rocks is much higher than previously described. A bimodal volcanic suite mixed with sediments is a geological environment which is regarded as favorable for both rich and large sulfide deposits. |
Blichfeldt, H.; Riiber, Carl C. , 1918 |
Rødfjeldets kisfelter. |
;Norges geologiske undersøkelse;FAGRAPPORT;Bergarkivet; No.BA 513;6 pages |
Abstract: | |
Rapporten frembyr forekomsten for salg til Norske Svolkisgruber A/S for kr. 180 000,-. Analyse av to prøver viser henholsvis 46,08 % S og 42,98 % S. Rapportens videre innhold er befaring av feltet med opplysning om geologi og utførte skjerpingsarbeider. Ialt 14 utmål omtales, og i to vises det til analyser, henholdsvis 48,50 % S - 0,12 % Cu og 40,92 % S og 0,24 % Cu. Driften på forekomsten forutsetter bygging av tanbane samt at alle rettigheter samles hos en eier. |
References not to be found in NGU's Reference Archive.: |
BNN A/S: Kjerneboringer. Diverse felt i Rana. Sølvberg, Breifonn, Rødvatn V. Heramb-Bertelberg, Hauknestind-Vatna. 1971-1986. BV3345 |
Marker, M. 1981: Oversigt over malmforekomster (skjerp) nord og øst for Rødvatnet. Upubl. rapp. |
Marker, M. 1981: Rødvatn-områdets geologi, Rana, Nordland, med særlig vekt på de strukturgeologiske træk. Upubl. rapp. |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||
NO0640.02 | Bedrock |
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NO0640.03 | Bedrock |
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NO0640.04 | Bedrock |
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NO0640.10 | Core |
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NO0640.11 | Core |
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RAH-02 | Dump |
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RAH-03 | Dump |
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NB! All analyse values are shown at the end of the printout.: |
Name of Locality : Skjerp 1 |
(Object Id : 1833,066,01,00) |
Location |
County : | Nordland (18) | Municipality : | Rana (1833) |
Map 1:50000: | Storforshei (2027-4) | Map 1:250000: | Mo i Rana |
Marking point: | Longitude: | 14.5872030 | Latitude: | 66.2904930 |
EU89-UTM Zone 33 | (Coordinates IS confirmed) |
X-coord: | 481478 m. | Y-coord: | 7352350 m. |
|
Commodity |
Main Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Sub Type: | Zinc | |
Element(s): | Kis Zn Pb |
Production |
Activity: | Pitting | Reserves: | ||
Prod. method: | Production: | |||
Prod. status: | Volume of dump: |
Structures |
Location: | Type: | Orientation(360 gr.): | Relation to min.: | |
Host rock | Foliation | Strike/Dip :274 / 80 | Post-mineralisation ;...Effect :Controls |
Information(s) in free text format |
Free text |
Liten røsk med grøft mot nord, ca 8 m lang. Mineralisering består vesentlig av svak pyritt-pyrrhotitt impregnasjon i amfibol-biotitt-kvartsgneiss. |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||
NO0640.01 | Bedrock |
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RAH-01 | Dump |
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NB! All analyse values are shown at the end of the printout.: |
Name of Locality : Skjerp 3 |
(Object Id : 1833,066,03,00) |
Location |
County : | Nordland (18) | Municipality : | Rana (1833) |
Map 1:50000: | Storforshei (2027-4) | Map 1:250000: | Mo i Rana |
Marking point: | Longitude: | 14.5839780 | Latitude: | 66.2905750 |
EU89-UTM Zone 33 | (Coordinates IS confirmed) |
X-coord: | 481333 m. | Y-coord: | 7352361 m. |
|
Commodity |
Main Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Sub Type: | Zinc | |
Element(s): | Kis Zn Pb |
Production |
Activity: | Pitting | Reserves: | ||
Prod. method: | Production: | |||
Prod. status: | Volume of dump: |
Structures |
Location: | Type: | Orientation(360 gr.): | Relation to min.: | |
Host rock | Foliation | Strike/Dip :110 / 80 | Post-mineralisation ;...Effect :Controls | |
Host rock | Fold axis | Dir./Plunge :280 / 45 | Post-mineralisation ;...Effect :Modifies |
Information(s) in free text format |
Free text |
4 m lang, 1 m bred og inntil 1.5 m dyp røsk. Vesentlig pyrittimpregnert kvarts-sericittskifer, dels i semimassive striper. Staurolitt er vanlig i 1-2 mm brune korn. |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||
NO0640.05 | Bedrock |
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NO0640.06 | Bedrock |
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RAH-04 | Dump |
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NB! All analyse values are shown at the end of the printout.: |
Name of Locality : Skjerp 4 |
(Object Id : 1833,066,04,00) |
Location |
County : | Nordland (18) | Municipality : | Rana (1833) |
Map 1:50000: | Storforshei (2027-4) | Map 1:250000: | Mo i Rana |
Marking point: | Longitude: | 14.5807600 | Latitude: | 66.2905750 |
EU89-UTM Zone 33 | (Coordinates IS confirmed) |
X-coord: | 481188 m. | Y-coord: | 7352361 m. |
|
Commodity |
Main Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Sub Type: | Zinc | |
Element(s): | Kis Zn Pb |
Production |
Activity: | Pitting | Reserves: | ||
Prod. method: | Production: | |||
Prod. status: | Volume of dump: | 35 m3 |
Structures |
Location: | Type: | Orientation(360 gr.): | Relation to min.: | |
Host rock | Foliation | Strike/Dip :249 / 70 | Post-mineralisation ;...Effect :Controls | |
Host rock | Fold axis | Dir./Plunge :285 / 40 | Post-mineralisation ;...Effect :Modifies |
Information(s) in free text format |
Free text |
Ca 10 m lang, 4 m bred og inntil 4 m dyp skjæring. Mineralisering av tynne striper med impregnasjon til semimassiv pyritt i kvarts-sericittskifer, dels biotittrik. Tett småfoldet. Partier sentralt i skjæringen er nesten ren sericitt med spredte 1-2 mm pyrittkorn. |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||
NO0640.07 | Bedrock |
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NO0640.08 | Bedrock |
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RAH-05 | Bedrock |
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NB! All analyse values are shown at the end of the printout.: |
Name of Locality : Skjerp 5 |
(Object Id : 1833,066,05,00) |
Location |
County : | Nordland (18) | Municipality : | Rana (1833) |
Map 1:50000: | Storforshei (2027-4) | Map 1:250000: | Mo i Rana |
Marking point: | Longitude: | 14.5798930 | Latitude: | 66.2904200 |
EU89-UTM Zone 33 | (Coordinates IS confirmed) |
X-coord: | 481149 m. | Y-coord: | 7352344 m. |
|
Commodity |
Main Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Sub Type: | Zinc | |
Element(s): | Kis Zn Pb |
Production |
Activity: | Pitting | Reserves: | ||
Prod. method: | Production: | |||
Prod. status: | Volume of dump: |
Structures |
Location: | Type: | Orientation(360 gr.): | Relation to min.: | |
Host rock | Foliation | Strike/Dip :250 / 65 | Post-mineralisation ;...Effect :Controls |
Information(s) in free text format |
Free text |
10 m lang og inntil 1 m dyp røskegrøft, 5 m3 tipp. Svak pyrittimpregnasjon i kvarts-sericittskifer. Like nord for røsken båndet med biotittrike lag. |
Name of Locality : Skjerp 6 |
(Object Id : 1833,066,06,00) |
Location |
County : | Nordland (18) | Municipality : | Rana (1833) |
Map 1:50000: | Storforshei (2027-4) | Map 1:250000: | Mo i Rana |
Marking point: | Longitude: | 14.5790450 | Latitude: | 66.2905080 |
EU89-UTM Zone 33 | (Coordinates IS confirmed) |
X-coord: | 481111 m. | Y-coord: | 7352355 m. |
|
Commodity |
Main Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Sub Type: | Zinc | |
Element(s): | Kis Zn Pb |
Production |
Activity: | Pitting | Reserves: | ||
Prod. method: | Production: | |||
Prod. status: | Volume of dump: | 15 m3 |
Information(s) in free text format |
Free text |
Seks mindre groper innenfor et område på 20 m (Ø-V) x 30 m (N-S). Lite å se, da gropene er dels gjenrast og overgrodd. Lengst SØ er det blokker med pyritt-impregnert kvarts-sericittskifer, dels i semimassive tynne årer med staurolitt. I de sentrale gropene biotittrik sericittskifer med spredt pyritt. |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||
NO0640.09 | Bedrock |
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RAH-06 | Dump |
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RAH-07 | Dump |
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NB! All analyse values are shown at the end of the printout.: |
Name of Locality : Skjerp 7 |
(Object Id : 1833,066,07,00) |
Location |
County : | Nordland (18) | Municipality : | Rana (1833) |
Map 1:50000: | Storforshei (2027-4) | Map 1:250000: | Mo i Rana |
Marking point: | Longitude: | 14.5786670 | Latitude: | 66.2904980 |
EU89-UTM Zone 33 | (Coordinates IS confirmed) |
X-coord: | 481095 m. | Y-coord: | 7352354 m. |
|
Commodity |
Main Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Sub Type: | Zinc | |
Element(s): | Kis Zn Pb |
Production |
Activity: | Pitting | Reserves: | ||
Prod. method: | Production: | |||
Prod. status: | Volume of dump: |
Information(s) in free text format |
Free text |
10 m vest for det sørligste skjerp i 6: 5 m lang gjenrast røsk. 2 m3 tipp. Pyritt-disseminert muskovittgneis. |
Analyse Results |
from |
Deposit Area 1833 - 066 Raudsandhaugen |
Element analyses |
( *=parts pr. million, #=parts pr.billion, Negative values means below detection limit value.) |
Sample No. | Sample Type | Cu* | Zn* | Pb* | Co* | Ni* | Ag* | Au# |
NO0640.01 | Bedrock | 243 | 280 | 1012 | 23 | 19 | 11.3 | 46.0 |
NO0640.02 | Bedrock | 224 | 29957 | 2399 | 10 | 3 | 34.9 | 173.0 |
NO0640.03 | Bedrock | 73 | 43946 | 4633 | 26 | 1 | 28.0 | 39.0 |
NO0640.04 | Bedrock | 25 | 18768 | 2590 | 15 | 4 | 26.6 | 77.0 |
NO0640.05 | Bedrock | 64 | 1064 | 99 | 30 | 5 | 9.7 | 109.0 |
NO0640.06 | Bedrock | 41 | 1393 | 69 | 20 | 4 | 3.7 | 61.0 |
NO0640.07 | Bedrock | 15 | 187 | 78 | 1 | 2 | 1.0 | 13.0 |
NO0640.08 | Bedrock | 88 | 178 | 10 | 9 | 1 | .9 | 3.0 |
NO0640.09 | Bedrock | 22 | 81 | 30 | 25 | 4 | 1.9 | 20.0 |
NO0640.10 | Core | 1119 | 742 | 124 | 29 | 7 | 3.5 | 63.0 |
NO0640.11 | Core | 714 | 797 | 250 | 29 | 4 | 2.1 | 24.0 |
RAH-01 | Dump | 251 | 522 | 329 | 30 | 23 | 1.0 | -10.0 |
RAH-02 | Dump | 155 | 41500 | 1820 | 12 | -5 | 11.0 | 290.0 |
RAH-03 | Dump | 99 | 3560 | 112 | 23 | -5 | 3.0 | 200.0 |
RAH-04 | Dump | 107 | 2680 | 106 | 8 | -5 | 2.0 | 50.0 |
RAH-05 | Bedrock | 27 | 531 | 263 | 3 | -5 | -1.0 | 10.0 |
RAH-06 | Dump | 56 | 2910 | 101 | 19 | -5 | 1.0 | 10.0 |
RAH-07 | Dump | 102 | 674 | 197 | 20 | -5 | 1.0 | 10.0 |
------------------ |
Sample No. | Pt# | Pd# | As* | Cd* | Ba* | Mo* | Sn* | Sb* | Bi* |
NO0640.01 | 1.0 | 4.0 | 2 | 28.8 | 30 | 3.00 | 2 | 84 | |
NO0640.02 | 8.0 | 6.0 | 9 | 133.2 | 1 | 6.00 | 2 | 54 | |
NO0640.03 | 1.0 | 1.0 | 18 | 187.8 | 2 | 7.00 | 11 | 80 | |
NO0640.04 | 1.0 | 7.0 | 12 | 67.2 | 1 | 5.00 | 2 | 45 | |
NO0640.05 | 1.0 | 6.0 | 20 | .2 | 2 | 6.00 | 2 | 9 | |
NO0640.06 | 1.0 | 1.0 | 19 | 16.8 | 2 | 6.00 | 2 | 5 | |
NO0640.07 | 1.0 | 2.0 | 4 | .5 | 44 | 1.00 | 2 | 8 | |
NO0640.08 | 1.0 | 5.0 | 2 | .3 | 94 | 1.00 | 2 | 3 | |
NO0640.09 | 1.0 | 2.0 | 2 | .2 | 5 | 8.00 | 2 | 5 | |
NO0640.10 | 18.0 | 20.0 | 12 | 4.8 | 7 | 3.00 | 2 | 2 | |
NO0640.11 | 6.0 | 2.0 | 7 | 3.6 | 6 | 5.00 | 2 | 2 | |
RAH-01 | 719 | 5.00 | 4 | ||||||
RAH-02 | 8 | 26.00 | 1 | ||||||
RAH-03 | 29 | 22.00 | 1 | ||||||
RAH-04 | 385 | 4.00 | 5 | ||||||
RAH-05 | 469 | 2.00 | 4 | ||||||
RAH-06 | 487 | 7.00 | 4 | ||||||
RAH-07 | 424 | -2.00 | 2 |
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Sample No. | S% | V* | Cr* | Mn* | Fe% | Th* | U* | W* | Sr* |
NO0640.01 | 4.15 | 47 | 12 | 341 | 6.91 | 7.00 | 5.00 | 1 | 5.0 |
NO0640.02 | 50.83 | 9 | 2 | 262 | 18.30 | 1.00 | 5.00 | 118 | 2.0 |
NO0640.03 | 48.66 | 7 | 3 | 347 | 19.54 | 3.00 | 5.00 | 153 | 2.0 |
NO0640.04 | 50.79 | 4 | 2 | 283 | 19.50 | 1.00 | 5.00 | 74 | 2.0 |
NO0640.05 | 36.05 | 1 | 3 | 238 | 19.43 | 1.00 | 5.00 | 3 | 1.0 |
NO0640.06 | 34.30 | 1 | 5 | 216 | 19.17 | 1.00 | 5.00 | 3 | 1.0 |
NO0640.07 | 1.65 | 1 | 9 | 230 | 1.94 | 1.00 | 5.00 | 1 | 2.0 |
NO0640.08 | 1.26 | 24 | 7 | 332 | 3.10 | 6.00 | 5.00 | 1 | 7.0 |
NO0640.09 | 17.76 | 3 | 6 | 208 | 18.45 | 2.00 | 5.00 | 1 | 1.0 |
NO0640.10 | 10.09 | 59 | 9 | 514 | 13.31 | 1.00 | 5.00 | 1 | 2.0 |
NO0640.11 | 12.19 | 28 | 8 | 470 | 14.94 | 1.00 | 5.00 | 1 | 3.0 |
RAH-01 | 30 | 1626 | 8.37 | 4.00 | 4.00 | ||||
RAH-02 | -10 | 620 | 37.70 | -1.00 | 2.00 | ||||
RAH-03 | -10 | 155 | 35.65 | -1.00 | -1.00 | ||||
RAH-04 | 10 | 387 | 7.53 | 1.00 | 1.00 | ||||
RAH-05 | 10 | 852 | 3.04 | 3.00 | 1.00 | ||||
RAH-06 | 10 | 465 | 12.65 | 2.00 | 2.00 | ||||
RAH-07 | 10 | 2246 | 7.11 | 8.00 | 2.00 |
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Sample No. | La* | B* | |||||||
NO0640.01 | 10.00 | 7 | |||||||
NO0640.02 | 2.00 | 23 | |||||||
NO0640.03 | 2.00 | 48 | |||||||
NO0640.04 | 2.00 | 20 | |||||||
NO0640.05 | 2.00 | 21 | |||||||
NO0640.06 | 2.00 | 19 | |||||||
NO0640.07 | 2.00 | 2 | |||||||
NO0640.08 | 2.00 | 2 | |||||||
NO0640.09 | 2.00 | 18 | |||||||
NO0640.10 | 2.00 | 2 | |||||||
NO0640.11 | 4.00 | 2 | |||||||
RAH-01 | |||||||||
RAH-02 | |||||||||
RAH-03 | |||||||||
RAH-04 | |||||||||
RAH-05 | |||||||||
RAH-06 | |||||||||
RAH-07 |
The fact sheet was created on 22.11.2024 |
Questions or comments regarding the fact sheet can be emailed to: ressursdatabaser@ngu.no |
Copyright © 2024 Geological Survey of Norway |