Norsk versjon | |||||
THE INDUSTRIAL MINERAL DATABASE | |||||
Deposit 1826 - 310 Ivarrud | |||||
(Object Id: 7708) (Last updated: 10.02.2017) |
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Location |
County: | Nordland | Municipality: | Aarborte (1826) |
Map 1:50000: | Susendalen (1925-1) | Map 1:250000: | Mosjøen |
Coordinate system: | EU89-UTM Zone 33 |
East: | 451432 m. | North: | 7255998 m. |
Longitude: | 13.9534610 | Latitude: | 65.4229690 |
Show on map |
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Resource |
Resource Type: | Carbonates | Resource Subtype: | Dolomite |
Importance |
Raw material meaning: | Local Importance (reg. 10.02.2015) |
Resources and production |
Activity: | Exploration | Reserves: | ||
Operating method: | Historical production: |
Products |
Element/product | Crude ore grade or quality | Reg. date | |
Agricultural lime | 11.12.2000 | ||
Filler | 11.12.2000 | ||
Flux | 19.12.2000 | ||
Metallurgical use | 19.12.2000 |
Operations |
From - To | Activity | Comments | |
1977 - 1977 | Geochemistry | ||
1977 - 1977 | Sampling | Company/Institution :NGU |
Mineralization |
Era: | Paleozoic | Period: | ||
Genesis: | Sedimentary/metamorphic | Form: | Layer | |
Main texture: | Banded | Min. distribution: |
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: | Helgeland Nappe Complex | |
Tectonic complex: | ||
Igneous complex: |
Group: | Formation: |
Mineralogy |
Mineral | Amount | |
Dolomite | Major mineral (>90%) | |
Mica | Subordinate mineral (1-10%) | |
Feldspar | Subordinate mineral (1-10%) | |
Quartz | Subordinate mineral (1-10%) | |
Calcite | Subordinate mineral (1-10%) | |
Pyrite | Accessory mineral (<1%) | |
Titanite | Accessory mineral (<1%) | |
Apatite | Accessory mineral (<1%) | |
Tremolite | Accessory mineral (<1%) | |
Chlorite | Accessory mineral (<1%) | |
Epidote | Accessory mineral (<1%) |
Information(s) in free text format |
Free text |
O. Ø.: Forekomstene er rapportert av O.Ø. Det gjelder alle i Hattfjelldalen. Fra noen av dem er det analyser. Kalken er finkornet og hvit. Forekomsten er også benevnt IVARRUD. Den er arbeidet med bl.a. av Elkem. Det er også gjort brennforsøk på prøver fra forekomsten. NGU rapp. 1556/4C. I.L.: Forekomsten ligger i Hattfjelldalen men i et annet dekke enn i det brede kalkdraget sørover Hattfjelldalen. På O. Ø. kart i rapporten tilsvarer dette omtrent hans område VII. Prøvene er tatt der det er blotninger. Det er kanskje en del plukkprøver og ikke representative prøver. Prøvepunktene er merket på kart i M 1:5 000. Analyse av 17 prøver viser at de fleste av prøvene er dolomitter. Mange av dem har god kjemi med lavt SiO2 innhold. O. Ø. beskriver dolomitten som inhomogen med innblanding av skiferlag. Analysene er gitt i rapporten som finnes i SSF arkiv. Befaring 24.9.01: Selve forekomsten på privat grunn. Mot NØ på vestsiden av Vefsna går den inn på Statsgrunn. Meget stort område med hvit til svakt grå dolomitt. Det samme som Surmyra. |
Bibliography: |
From NGU's Reference Archive: |
Bøckman, K.L. , 1967 |
Norges kalksteins- og kvartsforekomster. |
;Elektrokemisk A/S;FAGRAPPORT; UTREDNINGSRAPPORT;Bergarkivet; No.BA 5245;89 + 61 pages |
Strand, Trygve , 1953 |
Geologiske undersøkelser i den sydøstligste del av Helgeland. |
;Norges geologiske undersøkelse;TIDSSKRIFTARTIKKEL;NGU; No.184;124-141 pages |
Abstract: | |
Helgeland is the southern part of northern Norway. The writer and his assistants have worked in the northern part of the area shown on the map, the southern part of the same map is based upon the geological maps in manuscript of the late state-geologist Steinar Foslie. Foslie's working area was the Grong District, the north-easternmost part of southern Norway, known for its large pyrite deposits. The thrust-line on the map, fig. 1, separates a western and tectonically higher complex of highly metamorphosed rocks, including much of granites and gneisses, from an eastern and tectonically underlying complex of less metamorphosed rocks. The thrust is a tectonic feature of very great magnitude. The present paper deals with the rocks of the eastern complex only. In this complex the lowermost unit is the granitic massif of Store Børgefjell, of Precambrian age, according to G. Kautsky (1948). There seems to be little left of the autochtonous cover of the massif, the greater part of the rocks of the eastern area belonging to a thrust-sheet, the Seve nappe. In the area about 64 degrees 48'N, 13 degrees 53'E a series of phyllites and quartz-schists, the Røyrvik series of Foslie, contains a limestone in its lower part, and greenstone (meta-basalt) interbedded at two horizons. |
Strand, Trygve , 1955 |
Sydøstligste Helgelands geologi. |
;Norges geologiske undersøkelse;TIDSSKRIFTARTIKKEL;NGU; No.191;56-70 pages |
Abstract: | |
Geology of the south-eastermost part of Helgeland: Helgeland is the southern part of northern Norway. The present paper is a preliminary report presenting the results of mapping work during the summers 1951-54 by the writer and his assistants. A report based upon this work in 1951-52 has been published earlier (Strand 1953). The rocks in the area can be divided into four main units. The basal massif of Store Børgefjell is built of granitic gneisses, schists and, subordinately, of quartzites. Zones of feldspatiferous porphyroblast schists form a transition between the sedimentary schists and the granitic gneisses and indicate a granitization origin of the latter. On Swedish territory, according to G. Kautsky, the rocks of the Børgefjell amssif are normally overlain by Cambrian sediments of foreland type. This indicates a Pre-Cambrian age of the massif. On Norwegian side no rocks of a corresponding autochtonous or parautochtonous sedimentarty cover have been recognized. The sediments next above the massif have tectonic boundaries and form a tectonic unit composed of four stratigraphic divisions. |
Korneliussen, Are ; Gautneb, Håvard ; Raaness, Agnes , 2008 |
Karakterisering av karbonatforekomster i Nordland |
;Norges geologiske undersøkelse;RAPPORT;NGU-rapport; No.2008.041;93 s. pages |
Abstract: | |
Karbonatforekomster er bergarter som har høyt innhold av karbonatmineralene kalkspat og dolomitt. Slike bergarter har i mange tilfeller gjennomgått en kompleks geologisk utvikling, noe som har resultert i forekomster med stor spennvidde i karakteristika og egnethet for forskjellige anvendelser. Karbonatbergarter i form av forskjellige varianter av kalkstein, kalkspatmarmor, dolomitt og dolomittmarmor er karakteristiske bergartstyper i visse deler av Norge. Ressursgrunnlaget i Nordland er betydelig og en kan forvente at gruvedrift på karbonatforekomster, særlig kalkstein og kalkspatmarmor, vil få stor betydning også i framtiden. Til sammen er det drift på 22 karbonatforekomster i Norge, hvorav 6 i Nordland. Formålet med rapporten er å belyse nye muligheter som kan stimulere til ny aktivitet og verdiskaping. Arbeidet er utført i form av et sammenliknende kjemisk og mineralogisk studium av karbonatprøver fra ulike deler av fylket. Prøveutvalget omfatter både forekomster som er ansett som viktige i dagens situasjon og forekomster som hittil ikke har vært særlig påaktet. Et felleskrav for bruk av karbonater til industrielle formål er lavt innhold av jern både i bergart og mineraler. Langt flere forekomster enn forventet inneholder kalkspat og/eller dolomitt med lavt jerninnhold. Det betyr at det ved oppredning kan være mulig å produsere kalk av høy kvalitet fra eventuelle "nye" forekomster som tidligere ikke har vært ansett som interessante til industrielle formål. Ut fra de data som foreligger er de mest interessante regionene for kalkspatmarmor i Nordland (1) Ytre Helgeland inkl. Brønnøyområdet hvor Brønnøy Kalk har drift på Akselbergforekomsten og (2) Ofoten/Evenes-regionen som strekker seg inn i Sør-Troms (også kalt Ofoten - Sør-Troms regionen). Disse regionene krever særskilt oppfølging i form av nye undersøkelser for å oppnå bedre oversikt over ressursgrunnlaget. |
Øvereng, Odd , 1978 |
Kalkstein/dolomitt i Hattfjelldal-Susendalområdet, Nordland. |
;Norges geologiske undersøkelse;FAGRAPPORT;NGU-rapport; No.1556/4C;15 pages |
Abstract: | |
De utførte befaringene i Hattfjelldal-Susendalområdet er et ledd i den sys- tematiske registreringen av kalkstein og dolomitt i Nord-Norge. Hensikten var å fremskaffe en "røff" oversikt over de kvaliteter som måtte finnes innenfor det gigantiske karbonatmassivet som ligger i Hattfjelldal- Susendalområdet. Undersøkelsene viser at "komplekset" består av en intim sammenblanding av kalkstein og dolomitt. Analyseresultatene viser at kvaliteten er meget ujevn og stort sett dårlig, bortsett fra i en dolomittforekomst ved Ivar- rud. Denne forekomsten vil bli undersøkt nærmere sommeren 1978. |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||
NO0409.1 | Hand specimen |
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NO0409.10 | Hand specimen |
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NO0409.11 | Hand specimen |
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NO0409.12 | Hand specimen |
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NO0409.13 | Hand specimen |
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NO0409.14 | Hand specimen |
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NO0409.15 | Hand specimen |
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NO0409.16 | Hand specimen |
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NO0409.17 | Hand specimen |
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NO0409.18 | Hand specimen |
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NO0409.19 | Bedrock |
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NO0409.2 | Bedrock |
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NO0409.20 | Hand specimen |
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NO0409.21 | Hand specimen |
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NO0409.22 | Hand specimen |
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NO0409.23 | Hand specimen |
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NO0409.24 | Hand specimen |
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NO0409.25 | Hand specimen |
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NO0409.26 | Hand specimen |
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NO0409.27 | Hand specimen |
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NO0409.28 | Hand specimen |
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NO0409.29 | Hand specimen |
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NO0409.3 | Hand specimen |
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NO0409.30 | Hand specimen |
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NO0409.31 | Hand specimen |
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NO0409.32 | Hand specimen |
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NO0409.33 | Hand specimen |
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NO0409.34 | Hand specimen |
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NO0409.35 | Hand specimen |
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NO0409.36 | Hand specimen |
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NO0409.37 | Hand specimen |
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NO0409.38 | Hand specimen |
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NO0409.39 | Hand specimen |
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NO0409.4 | Hand specimen |
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NO0409.40 | Hand specimen |
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NO0409.41 | Hand specimen |
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NO0409.42 | Hand specimen |
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NO0409.43 | Hand specimen |
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NO0409.44 | Hand specimen |
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NO0409.45 | Hand specimen |
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NO0409.46 | Hand specimen |
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NO0409.47 | Hand specimen |
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NO0409.48 | Hand specimen |
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NO0409.49 | Hand specimen |
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NO0409.5 | Hand specimen |
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NO0409.50 | Hand specimen |
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NO0409.51 | Hand specimen |
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NO0409.52 | Hand specimen |
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NO0409.53 | Hand specimen |
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NO0409.54 | Hand specimen |
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NO0409.55 | Hand specimen |
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NO0409.56 | Hand specimen |
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NO0409.57 | Hand specimen |
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NO0409.58 | Hand specimen |
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NO0409.59 | Hand specimen |
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NO0409.6 | Hand specimen |
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NO0409.60 | Hand specimen |
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NO0409.61 | Hand specimen |
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NO0409.62 | Hand specimen |
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NO0409.63 | Hand specimen |
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NO0409.64 | Hand specimen |
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NO0409.65 | Hand specimen |
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NO0409.66 | Hand specimen |
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NO0409.67 | Hand specimen |
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NO0409.68 | Hand specimen |
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NO0409.7 | Hand specimen |
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NO0409.8 | Hand specimen |
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NO0409.9 | Hand specimen |
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NB! All analyse values are shown at the end of the printout.: |
Name of Sample point: II |
(Object Id: 18295 310,00,01) |
|
Location |
County: | Nordland | Municipality: | Aarborte (1826) |
Map 1:50000: | Susendalen (1925-1) | Map 1:250000: | Mosjøen |
Coordinate system: | EU89-UTM Zone 33 |
East: | 452226 m. | North: | 7256511 m. |
Longitude: | 13.9703820 | Latitude: | 65.4276940 |
Show on map |
|
Resource |
Resource Type: | Carbonates | Resource Subtype: | Dolomite |
Information(s) in free text format |
Free text |
Prøve samlet inn av Ingvar Lindahl i 2006. |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||||
IL49 | Hand specimen |
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NB! All analyse values are shown at the end of the printout.: |
Name of Sample point: Il50 |
(Object Id: 18296 310,00,02) |
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Location |
County: | Nordland | Municipality: | Aarborte (1826) |
Map 1:50000: | Susendalen (1925-1) | Map 1:250000: | Mosjøen |
Coordinate system: | EU89-UTM Zone 33 |
East: | 452417 m. | North: | 7255843 m. |
Longitude: | 13.9747320 | Latitude: | 65.4217210 |
Show on map |
|
Resource |
Resource Type: | Carbonates | Resource Subtype: | Dolomite |
Information(s) in free text format |
Free text |
Prøve samlet inn av Ingvar Lindahl i 2006. |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||||
IL50 | Hand specimen |
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NB! All analyse values are shown at the end of the printout.: |
Analyse Results |
from |
Deposit Area 1826 - 310 Ivarrud |
Analysis of acid soluble CaO and Mgo |
Analyzed values | Derived values |
Sample No. | Sample Type | Acid soluble CaO | Acid soluble MgO | Dolomite | Calcite | Unsolved |
IL49 | Hand specimen | 27.42% | 20.39% | 93.26% | -1.68% | 8.42% |
IL50 | Hand specimen | 28.26% | 19.40% | 88.73% | 2.28% | 8.99% |
NO0409.1 | Hand specimen | 28.80% | 20.70% | 94.68% | .02% | 5.30% |
NO0409.10 | Hand specimen | 29.10% | 20.10% | 91.94% | 2.04% | 6.02% |
NO0409.11 | Hand specimen | 29.40% | 19.60% | 89.65% | 3.82% | 6.53% |
NO0409.12 | Hand specimen | 28.80% | 20.30% | 92.85% | 1.01% | 6.14% |
NO0409.13 | Hand specimen | 33.30% | 11.90% | 54.43% | 29.89% | 15.68% |
NO0409.14 | Hand specimen | 42.40% | 8.40% | 38.42% | 54.82% | 6.76% |
NO0409.15 | Hand specimen | 46.00% | 5.20% | 23.78% | 69.19% | 7.02% |
NO0409.16 | Hand specimen | 32.00% | 15.40% | 70.44% | 18.88% | 10.68% |
NO0409.17 | Hand specimen | 34.00% | 11.40% | 52.14% | 32.38% | 15.47% |
NO0409.18 | Hand specimen | 42.20% | 5.40% | 24.70% | 61.91% | 13.39% |
NO0409.19 | Bedrock | 34.80% | 11.60% | 53.06% | 33.31% | 13.63% |
NO0409.2 | Bedrock | 29.20% | 20.80% | 95.14% | .48% | 4.38% |
NO0409.20 | Hand specimen | 35.50% | 10.60% | 48.48% | 37.05% | 14.47% |
NO0409.21 | Hand specimen | 30.40% | 14.30% | 65.41% | 18.76% | 15.83% |
NO0409.22 | Hand specimen | 29.90% | 16.90% | 77.30% | 11.41% | 11.29% |
NO0409.23 | Hand specimen | 29.60% | 15.50% | 70.90% | 14.35% | 14.75% |
NO0409.24 | Hand specimen | 31.10% | 15.90% | 72.73% | 16.04% | 11.24% |
NO0409.25 | Hand specimen | 30.10% | 15.30% | 69.98% | 15.74% | 14.28% |
NO0409.26 | Hand specimen | 50.30% | 3.00% | 13.72% | 82.33% | 3.95% |
NO0409.27 | Hand specimen | 53.80% | 3.00% | 13.72% | 88.57% | -2.30% |
NO0409.28 | Hand specimen | 45.90% | 3.60% | 16.47% | 72.98% | 10.55% |
NO0409.29 | Hand specimen | 44.00% | 8.40% | 38.42% | 57.68% | 3.90% |
NO0409.3 | Hand specimen | 28.90% | 20.00% | 91.48% | 1.93% | 6.59% |
NO0409.30 | Hand specimen | 37.90% | 11.50% | 52.60% | 39.10% | 8.30% |
NO0409.31 | Hand specimen | 42.00% | 6.70% | 30.65% | 58.33% | 11.03% |
NO0409.32 | Hand specimen | 37.30% | 37.30% | 170.61% | -26.02% | -44.59% |
NO0409.33 | Hand specimen | 30.00% | 18.50% | 84.62% | 7.62% | 7.76% |
NO0409.34 | Hand specimen | 36.70% | 12.20% | 55.80% | 35.22% | 8.98% |
NO0409.35 | Hand specimen | 29.90% | 18.30% | 83.70% | 7.94% | 8.36% |
NO0409.36 | Hand specimen | 33.70% | 7.00% | 32.02% | 42.77% | 25.21% |
NO0409.37 | Hand specimen | 31.70% | 18.30% | 83.70% | 11.15% | 5.15% |
NO0409.38 | Hand specimen | 33.90% | 20.50% | 93.76% | 9.61% | -3.38% |
NO0409.39 | Hand specimen | .50% | 3.00% | 13.72% | -6.55% | 92.83% |
NO0409.4 | Hand specimen | 31.70% | 20.50% | 93.76% | 5.69% | .55% |
NO0409.40 | Hand specimen | 48.80% | 3.00% | 13.72% | 79.65% | 6.63% |
NO0409.41 | Hand specimen | 29.40% | 20.90% | 95.59% | .59% | 3.82% |
NO0409.42 | Hand specimen | 23.80% | 3.20% | 14.64% | 34.53% | 50.83% |
NO0409.43 | Hand specimen | 29.80% | 19.90% | 91.02% | 3.79% | 5.19% |
NO0409.44 | Hand specimen | 29.70% | 20.80% | 95.14% | 1.37% | 3.49% |
NO0409.45 | Hand specimen | 37.70% | 9.90% | 45.28% | 42.71% | 12.01% |
NO0409.46 | Hand specimen | 47.40% | 3.00% | 13.72% | 77.15% | 9.13% |
NO0409.47 | Hand specimen | 45.50% | 3.80% | 17.38% | 71.77% | 10.85% |
NO0409.48 | Hand specimen | 46.20% | 4.50% | 20.58% | 71.29% | 8.13% |
NO0409.49 | Hand specimen | 42.60% | 6.90% | 31.56% | 58.90% | 9.54% |
NO0409.5 | Hand specimen | 28.60% | 15.20% | 69.52% | 13.31% | 17.16% |
NO0409.50 | Hand specimen | 43.20% | 3.00% | 13.72% | 69.65% | 16.62% |
NO0409.51 | Hand specimen | 28.40% | 20.40% | 93.31% | .05% | 6.65% |
NO0409.52 | Hand specimen | 28.40% | 20.50% | 93.76% | -.20% | 6.44% |
NO0409.53 | Hand specimen | 28.20% | 18.50% | 84.62% | 4.41% | 10.98% |
NO0409.54 | Hand specimen | 20.10% | 21.30% | 97.42% | -17.00% | 19.58% |
NO0409.55 | Hand specimen | 28.70% | 17.50% | 80.04% | 7.78% | 12.18% |
NO0409.56 | Hand specimen | 29.10% | 20.50% | 93.76% | 1.05% | 5.19% |
NO0409.57 | Hand specimen | 28.40% | 19.40% | 88.73% | 2.53% | 8.74% |
NO0409.58 | Hand specimen | 28.30% | 21.10% | 96.51% | -1.87% | 5.36% |
NO0409.59 | Hand specimen | 29.10% | 21.30% | 97.42% | -.94% | 3.51% |
NO0409.6 | Hand specimen | 29.00% | 19.70% | 90.11% | 2.86% | 7.04% |
NO0409.60 | Hand specimen | 28.50% | 20.80% | 95.14% | -.77% | 5.63% |
NO0409.61 | Hand specimen | 28.70% | 20.30% | 92.85% | .83% | 6.32% |
NO0409.62 | Hand specimen | 29.30% | 20.70% | 94.68% | .91% | 4.41% |
NO0409.63 | Hand specimen | 29.10% | 18.40% | 84.16% | 6.26% | 9.58% |
NO0409.64 | Hand specimen | 27.90% | 19.70% | 90.11% | .89% | 9.00% |
NO0409.65 | Hand specimen | 29.50% | 20.50% | 93.76% | 1.76% | 4.47% |
NO0409.66 | Hand specimen | 28.60% | 19.50% | 89.19% | 2.64% | 8.17% |
NO0409.67 | Hand specimen | 29.00% | 20.10% | 91.94% | 1.86% | 6.20% |
NO0409.68 | Hand specimen | 28.80% | 19.50% | 89.19% | 2.99% | 7.81% |
NO0409.7 | Hand specimen | 29.90% | 21.10% | 96.51% | .99% | 2.50% |
NO0409.8 | Hand specimen | 29.90% | 19.70% | 90.11% | 4.46% | 5.43% |
NO0409.9 | Hand specimen | 31.60% | 19.30% | 88.28% | 8.49% | 3.24% |
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* | As* |
IL49 | Hand specimen | -2 | 3 | 4 | -4 | -2 | -10.0 | -10 |
IL50 | Hand specimen | -2 | 3 | 4 | -4 | -2 | -10.0 | -10 |
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Sample No. | Cd* | Ba* | Mo* | Sn* | Sb* | Bi* | Se* | Ga* | Ge* |
IL49 | -10.0 | -10 | -1.00 | -5 | -10 | -5 | 2.20 | -1.00 | -1.00 |
IL50 | -10.0 | -10 | -1.00 | -5 | -10 | -5 | -2.00 | -1.00 | -1.00 |
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Sample No. | V* | Cr* | Th* | U* | W* | Rb* | Sr* | Y* | Zr* |
IL49 | -5 | -4 | -4.00 | -2.00 | -5 | -1.0 | 57.0 | -1.0 | -1 |
IL50 | -5 | -4 | -4.00 | -2.00 | -5 | -1.0 | 110.0 | -1.0 | -1 |
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Sample No. | Nb* | Ta* | Cs* | La* | Ce* | Nd* | Sm* | Yb* | Sc* |
IL49 | -1.00 | -4.00 | -10.00 | -10.00 | -20.00 | -10.00 | -10.00 | -5.00 | -15.00 |
IL50 | -1.00 | -4.00 | -10.00 | -10.00 | -20.00 | -10.00 | -10.00 | -5.00 | -15.00 |
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Sample No. | Te* | Hf* | Hg* | Tl* | |||||
IL49 | -10.00 | -5.00 | -4 | 6 | |||||
IL50 | -10.00 | -5.00 | -4 | -5 |
Oxide analyses |
( All values are in % ) |
Sample No. | Sample Type | SiO2 | Al2O3 | TiO2 | Fe2O3 | MnO | MgO | CaO |
IL49 | Hand specimen | 0.09 | 0.02 | 0.00 | 22.48 | 30.91 | ||
IL50 | Hand specimen | 0.65 | 0.03 | 0.00 | 21.46 | 32.02 | ||
NO0409.1 | Hand specimen | 0.85 | 0.12 | 0.02 | 0.14 | -0.01 | 20.26 | 30.32 |
NO0409.10 | Hand specimen | 0.65 | 0.13 | 0.02 | 0.20 | 0.01 | 20.68 | 30.18 |
NO0409.11 | Hand specimen | 0.35 | 0.10 | 0.02 | 0.15 | -0.01 | 20.40 | 30.00 |
NO0409.12 | Hand specimen | 0.89 | 0.11 | 0.02 | 0.13 | 0.01 | 20.58 | 29.18 |
NO0409.13 | Hand specimen | 4.36 | 0.67 | 0.04 | 0.30 | -0.01 | 15.95 | 32.92 |
NO0409.14 | Hand specimen | 1.77 | 0.25 | 0.02 | 0.20 | 0.13 | 9.34 | 46.08 |
NO0409.15 | Hand specimen | 2.56 | 0.41 | 0.03 | 0.15 | 0.20 | 6.24 | 48.91 |
NO0409.16 | Hand specimen | 4.36 | 0.41 | 0.04 | 0.41 | 0.13 | 17.59 | 31.06 |
NO0409.17 | Hand specimen | 5.14 | 1.01 | 0.06 | 0.42 | 0.02 | 15.94 | 32.09 |
NO0409.18 | Hand specimen | 3.49 | 0.61 | 0.04 | 0.34 | 0.21 | 8.09 | 45.29 |
NO0409.19 | Bedrock | 6.61 | 1.23 | 0.07 | 0.41 | 0.16 | 13.72 | 33.67 |
NO0409.2 | Bedrock | 0.24 | 0.07 | 0.01 | 0.21 | -0.01 | 19.93 | 30.21 |
NO0409.20 | Hand specimen | 5.24 | 0.93 | 0.05 | 0.49 | 0.15 | 13.71 | 34.03 |
NO0409.21 | Hand specimen | 5.01 | 1.25 | 0.07 | 0.91 | 0.28 | 17.41 | 30.23 |
NO0409.22 | Hand specimen | 3.39 | 0.48 | 0.03 | 0.36 | 0.04 | 18.58 | 29.81 |
NO0409.23 | Hand specimen | 5.20 | 0.91 | 0.07 | 0.51 | 0.12 | 18.51 | 29.09 |
NO0409.24 | Hand specimen | 3.04 | 0.80 | 0.05 | 0.58 | 0.15 | 18.06 | 31.02 |
NO0409.25 | Hand specimen | 4.33 | 0.91 | 0.06 | 0.40 | 0.17 | 18.06 | 29.82 |
NO0409.26 | Hand specimen | 2.20 | 0.34 | 0.02 | 0.13 | 0.51 | 1.77 | 52.76 |
NO0409.27 | Hand specimen | 1.91 | 0.25 | 0.02 | 0.11 | 0.26 | 1.53 | 53.33 |
NO0409.28 | Hand specimen | 4.51 | 0.98 | 0.05 | 0.27 | 0.08 | 3.84 | 47.89 |
NO0409.29 | Hand specimen | 3.14 | 0.57 | 0.04 | 0.26 | 0.26 | 8.81 | 44.82 |
NO0409.3 | Hand specimen | 0.10 | 0.04 | 0.01 | 0.15 | -0.01 | 20.63 | 29.12 |
NO0409.30 | Hand specimen | 2.72 | 0.26 | 0.02 | 0.21 | 0.08 | 13.60 | 34.88 |
NO0409.31 | Hand specimen | 6.16 | 0.64 | 0.04 | 0.36 | 0.26 | 1.44 | 44.30 |
NO0409.32 | Hand specimen | 6.93 | 0.91 | 0.05 | 0.42 | 0.34 | 10.51 | 40.84 |
NO0409.33 | Hand specimen | 0.58 | 0.41 | 0.02 | 0.29 | 0.04 | 19.14 | 30.31 |
NO0409.34 | Hand specimen | 1.42 | 0.42 | 0.03 | 0.37 | 0.11 | 12.88 | 41.46 |
NO0409.35 | Hand specimen | 0.56 | 0.02 | 0.01 | 0.20 | 0.01 | 19.71 | 29.74 |
NO0409.36 | Hand specimen | 9.71 | 2.18 | 0.15 | 0.92 | 1.41 | 9.01 | 30.06 |
NO0409.37 | Hand specimen | 2.16 | 0.86 | 0.02 | 0.32 | -0.01 | 21.16 | 31.49 |
NO0409.38 | Hand specimen | 1.46 | 0.30 | 0.03 | 0.27 | 0.01 | 21.17 | 32.06 |
NO0409.39 | Hand specimen | 52.90 | 17.91 | 0.79 | 8.28 | 2.96 | 4.10 | 5.16 |
NO0409.4 | Hand specimen | 0.45 | 0.19 | 0.02 | 0.24 | 0.05 | 19.79 | 31.81 |
NO0409.40 | Hand specimen | 5.51 | 0.31 | 0.01 | 0.23 | 0.08 | 2.14 | 50.64 |
NO0409.41 | Hand specimen | 0.06 | 0.06 | 0.01 | 0.20 | -0.01 | 20.82 | 29.17 |
NO0409.42 | Hand specimen | 23.09 | 0.11 | 0.01 | 1.19 | -0.01 | 18.41 | 27.59 |
NO0409.43 | Hand specimen | 0.82 | 0.24 | 0.02 | 0.24 | 0.01 | 20.26 | 30.03 |
NO0409.44 | Hand specimen | 0.37 | 0.16 | 0.02 | 0.27 | 0.07 | 20.22 | 29.67 |
NO0409.45 | Hand specimen | 3.37 | 0.25 | 0.01 | 0.29 | 0.01 | 13.20 | 42.44 |
NO0409.46 | Hand specimen | 4.05 | 0.70 | 48.60 | 0.27 | 0.03 | 5.75 | 5.75 |
NO0409.47 | Hand specimen | 4.48 | 0.90 | 0.06 | 0.36 | 0.52 | 5.77 | 48.26 |
NO0409.48 | Hand specimen | 2.80 | 0.41 | 0.02 | 0.19 | 0.14 | 5.26 | 49.63 |
NO0409.49 | Hand specimen | 1.74 | 0.21 | 0.01 | 0.20 | 0.06 | 0.56 | 38.84 |
NO0409.5 | Hand specimen | 5.89 | 0.89 | 0.06 | 0.32 | 0.36 | 18.47 | 29.88 |
NO0409.50 | Hand specimen | 7.28 | 1.37 | 0.01 | 0.51 | 0.69 | 5.74 | 46.46 |
NO0409.51 | Hand specimen | 1.09 | 0.41 | 0.03 | 0.29 | 0.08 | 20.67 | 28.81 |
NO0409.52 | Hand specimen | 0.61 | 0.10 | 0.01 | 0.14 | -0.01 | 20.64 | 30.19 |
NO0409.53 | Hand specimen | 0.92 | 0.43 | 0.03 | 0.33 | 0.06 | 20.69 | 29.61 |
NO0409.54 | Hand specimen | 0.79 | 0.16 | 0.02 | 0.16 | 0.03 | 20.86 | 30.24 |
NO0409.55 | Hand specimen | 0.38 | 0.18 | 0.02 | 0.21 | 0.01 | 21.10 | 29.91 |
NO0409.56 | Hand specimen | 0.61 | 0.34 | 0.04 | 0.27 | 0.01 | 20.48 | 29.22 |
NO0409.57 | Hand specimen | 2.54 | 0.79 | 0.05 | 0.34 | 0.02 | 19.42 | 29.72 |
NO0409.58 | Hand specimen | 0.76 | 0.24 | 0.03 | 0.17 | 0.04 | 20.26 | 29.69 |
NO0409.59 | Hand specimen | 0.34 | 0.19 | 0.02 | 0.16 | 0.03 | 20.18 | 29.37 |
NO0409.6 | Hand specimen | 0.55 | 0.16 | 0.02 | 0.18 | 0.02 | 21.03 | 29.52 |
NO0409.60 | Hand specimen | 1.51 | 0.37 | 0.03 | 0.21 | 0.07 | 19.62 | 30.17 |
NO0409.61 | Hand specimen | 0.63 | 0.32 | 0.03 | 0.19 | -0.01 | 20.10 | 29.62 |
NO0409.62 | Hand specimen | 0.52 | 0.13 | 0.02 | 0.16 | 0.02 | 20.70 | 29.53 |
NO0409.63 | Hand specimen | 0.37 | 0.08 | 0.01 | 0.13 | -0.01 | 19.87 | 30.46 |
NO0409.64 | Hand specimen | 1.25 | 0.60 | 0.03 | 0.24 | 0.08 | 20.21 | 29.43 |
NO0409.65 | Hand specimen | 0.53 | 0.19 | 0.02 | 0.15 | -0.01 | 19.79 | 30.39 |
NO0409.66 | Hand specimen | 0.93 | 0.21 | 0.02 | 0.16 | 0.03 | 19.97 | 29.71 |
NO0409.67 | Hand specimen | 1.98 | 0.26 | 0.03 | 0.16 | 0.02 | 19.50 | 29.09 |
NO0409.68 | Hand specimen | 2.02 | 0.18 | 0.02 | 0.16 | -0.01 | 20.48 | 30.11 |
NO0409.7 | Hand specimen | 0.32 | 0.18 | 0.02 | 0.21 | 0.03 | 20.16 | 30.19 |
NO0409.8 | Hand specimen | 0.78 | 0.21 | 0.02 | 0.23 | -0.01 | 20.61 | 30.17 |
NO0409.9 | Hand specimen | 0.61 | 0.17 | 0.02 | 0.22 | 0.02 | 20.19 | 29.52 |
------------------ |
Sample No. | Na2O | K2O | P2O5 | Sum | |||||
IL49 | -0.10 | 0.00 | -0.01 | 53.00 | |||||
IL50 | -0.10 | 0.00 | 0.02 | 54.00 | |||||
NO0409.1 | 0.01 | 0.05 | -0.10 | 52.00 | |||||
NO0409.10 | -0.01 | 0.04 | -0.10 | 52.00 | |||||
NO0409.11 | -0.01 | -0.01 | -0.10 | 51.00 | |||||
NO0409.12 | -0.01 | 0.04 | -0.10 | 51.00 | |||||
NO0409.13 | 0.01 | 0.05 | -0.10 | 54.00 | |||||
NO0409.14 | 0.05 | -0.01 | 0.40 | 58.00 | |||||
NO0409.15 | 0.01 | 0.01 | 0.60 | 59.00 | |||||
NO0409.16 | 0.01 | 0.04 | -0.10 | 54.00 | |||||
NO0409.17 | 0.02 | 0.05 | -0.10 | 55.00 | |||||
NO0409.18 | 0.04 | 0.01 | -0.10 | 58.00 | |||||
NO0409.19 | -0.01 | 0.05 | -0.10 | 56.00 | |||||
NO0409.2 | 0.01 | 0.04 | -0.10 | 51.00 | |||||
NO0409.20 | -0.01 | 0.05 | -0.10 | 55.00 | |||||
NO0409.21 | 0.01 | 0.05 | -0.10 | 55.00 | |||||
NO0409.22 | 0.02 | 0.05 | -0.10 | 53.00 | |||||
NO0409.23 | 0.02 | 0.05 | -0.10 | 54.00 | |||||
NO0409.24 | 0.01 | 0.05 | -0.10 | 54.00 | |||||
NO0409.25 | 0.01 | 0.05 | -0.10 | 54.00 | |||||
NO0409.26 | 0.01 | 0.01 | -0.10 | 58.00 | |||||
NO0409.27 | 0.04 | 0.01 | -0.10 | 57.00 | |||||
NO0409.28 | -0.01 | 0.02 | -0.10 | 58.00 | |||||
NO0409.29 | -0.01 | 0.01 | -0.10 | 58.00 | |||||
NO0409.3 | 0.01 | 0.03 | -0.10 | 50.00 | |||||
NO0409.30 | 0.02 | 0.05 | -0.10 | 52.00 | |||||
NO0409.31 | 0.06 | -0.01 | 0.30 | 54.00 | |||||
NO0409.32 | 0.02 | -0.01 | -0.10 | 60.00 | |||||
NO0409.33 | 0.02 | 0.04 | -0.10 | 51.00 | |||||
NO0409.34 | -0.01 | -0.01 | -0.10 | 57.00 | |||||
NO0409.35 | -0.01 | 0.05 | -0.10 | 50.00 | |||||
NO0409.36 | 0.03 | 0.03 | -0.10 | 53.00 | |||||
NO0409.37 | 0.05 | 0.05 | -0.10 | 56.00 | |||||
NO0409.38 | 0.05 | 0.05 | -0.10 | 55.00 | |||||
NO0409.39 | 0.14 | 0.38 | -0.10 | 93.00 | |||||
NO0409.4 | 0.03 | -0.01 | -0.10 | 52.00 | |||||
NO0409.40 | 0.03 | -0.01 | -0.10 | 59.00 | |||||
NO0409.41 | -0.01 | 0.05 | -0.10 | 50.00 | |||||
NO0409.42 | 0.10 | 0.04 | -0.10 | 70.00 | |||||
NO0409.43 | 0.01 | 0.04 | -0.10 | 52.00 | |||||
NO0409.44 | 0.01 | 0.05 | -0.10 | 51.00 | |||||
NO0409.45 | 0.02 | 0.10 | -0.10 | 60.00 | |||||
NO0409.46 | 0.05 | 0.01 | -0.10 | 65.00 | |||||
NO0409.47 | 0.04 | 0.03 | -0.10 | 60.00 | |||||
NO0409.48 | 0.05 | 0.06 | -0.10 | 58.00 | |||||
NO0409.49 | 0.08 | 0.03 | -0.10 | 42.00 | |||||
NO0409.5 | 0.01 | 0.02 | -0.10 | 56.00 | |||||
NO0409.50 | 0.02 | 0.03 | -0.10 | 62.00 | |||||
NO0409.51 | -0.01 | 0.04 | -0.10 | 51.00 | |||||
NO0409.52 | -0.01 | 0.04 | -0.10 | 52.00 | |||||
NO0409.53 | -0.01 | 0.04 | -0.10 | 52.00 | |||||
NO0409.54 | -0.01 | 0.05 | -0.10 | 52.00 | |||||
NO0409.55 | -0.01 | 0.05 | -0.10 | 52.00 | |||||
NO0409.56 | -0.01 | 0.05 | -0.10 | 51.00 | |||||
NO0409.57 | -0.01 | 0.05 | -0.10 | 53.00 | |||||
NO0409.58 | -0.01 | 0.04 | -0.10 | 51.00 | |||||
NO0409.59 | -0.01 | 0.05 | -0.10 | 50.00 | |||||
NO0409.6 | -0.01 | -0.01 | -0.10 | 51.00 | |||||
NO0409.60 | -0.01 | 0.05 | -0.10 | 52.00 | |||||
NO0409.61 | -0.01 | 0.05 | -0.10 | 51.00 | |||||
NO0409.62 | -0.01 | 0.05 | 0.30 | 51.00 | |||||
NO0409.63 | -0.01 | 0.04 | -0.10 | 51.00 | |||||
NO0409.64 | 0.01 | 0.05 | -0.10 | 52.00 | |||||
NO0409.65 | 0.01 | 0.04 | -0.10 | 51.00 | |||||
NO0409.66 | -0.01 | 0.05 | -0.10 | 51.00 | |||||
NO0409.67 | -0.01 | 0.05 | -0.10 | 51.00 | |||||
NO0409.68 | -0.01 | 0.05 | -0.10 | 53.00 | |||||
NO0409.7 | 0.01 | 0.05 | -0.10 | 51.00 | |||||
NO0409.8 | 0.01 | 0.03 | -0.10 | 52.00 | |||||
NO0409.9 | -0.01 | 0.04 | -0.10 | 51.00 |
The fact sheet was created on 19.04.2024 |
Questions or comments regarding the fact sheet can be emailed to: ressursdatabaser@ngu.no |
Copyright © 2024 Geological Survey of Norway |