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MALMDATABASEN | |||||
Forekomstområde 1845 - 014 | |||||
(Sist oppdatert 23.okt.2024) |
Navn på forekomstområde : Gjerdalsvann |
(Objekt Id : 1845,014,00,00) |
Lokalisering |
Fylke : | Nordland (18) | Kommune : | Sørfold (1845) |
Kart 1:50000: | Gjerdal (2130-2) | Kart 1:250000: | Sulitjelma |
Markeringspunkt: | Lengdegrad: | 16.1356130 | Breddegrad: | 67.6945320 |
EU89-UTM Zone 33 | (Koordinatene ER bekreftet) |
X-koord: | 548097 m. | Y-koord: | 7509248 m. |
|
Materialtype |
Hovedtype: | Spesialmetaller (Nb,Ta,Be,Li,Sc,REE) | Subtype: | REE-metaller | |
Element(er): | La Ce Nb Y U Th |
Produksjon |
Aktivitet: | Prospektering | Reserver: | ||
Prod. metode: | Produksjon: | |||
Prod. status: | Tippvolum: |
Betydning |
Offentlig: | (Ingen data) |
Økonomisk: | Ikke vurdert |
Mineralisering |
Æra: | Periode: | |||
Datering: | Metode: | |||
Genese: | Form: | |||
Hovedtextur: | Min. fordeling: |
Kornstørrelse: | Hovedomvandling: |
Strøk/Fall: | Retning: | |||
Feltstupning: |
Stratigrafisk klassifikasjon av vertsbergart |
Æra: | Periode: |
Provins: | ||
Geotek.enhet: | ||
Tektonisk complex: | ||
Intrusivt komplex: |
Gruppe: | Formasjon: |
Opplysning(er) i fritekstformat |
Fri tekst |
Müller (2011) write the following: The Gjerdalsvatn locality was chosen as target area on the basis of one Uranal database analysis of granite gneiss with anomalously high La - 541 ppm and Ce - 1200 ppm (Müller 2010). The sample was collected by J. Hysingjord in the 1970s. The locality was immediately identified in the field because of high gamma-radiation of >700 cps compared to the host granite gneiss with about 400 cps. The rock with the high gamma-radiation forms a dyke-like structure which is about 600 m long and up to 20 m wide and plunges 60-70º to the S-SE (Figs. 21, 22). The estimated resource is about 150 000 tons assuming a vertical extension of the mineralisation of 25 m. It is a fine-grained, almost aplitic biotite granite gneiss which can be easily distinguished from the coarse-grained granite gneiss host (Fig. 22b). Four finegrained granite gneiss samples (23091001, -02, -04, 28091009) and one coarse-grained granite gneiss sample (23091003) were collected. Surprisingly, the host granite gneiss (sample 23091003) has the highest REO+Y2O3 of 0.111 wt.% but the lowest U - 4 ppm and Th of 30 ppm, explaining the low gamma-ray intensity (Fig. 23). The fine-grained granite gneiss contain 0.010 to 0.052 wt.% REO+Y2O3, 164 - 230 ppm Zr, 38-56 ppm Th and 5 - 21 ppm U. In this case, the scintillometer measurements are not indicative for elevated REE concentrations. The Gjerdalsvatn granite gneisses are slightly enriched in LREE compared to average granite composition and slightly depleted in HREE (Fig. 24). Sample 28091009 is, for some reason, depleted in all REE compared to the average granite composition. The most common REE-bearing accessory minerals are allanite (20-250 µm), zircon (20-120 µm) and apatite (40-100 µm) (Fig. 25). The LREE enrichment is explained by the dominance of allanite and apatite over zirco |
Litteraturfortegnelser: |
Fra NGU's Referansearkiv.: |
Müller, Axel , 2011 |
Potential of rare earth element and Zr-, Be, U-, Th-, (W-) mineralisations in central and northern Nordland - Part 2 |
;Norges geologiske undersøkelse;RAPPORT;NGU-rapport; No.2011.021;56 sider |
Abstrakt: | |
In this report results of the investigation of potential rare earth elements (REE) and Zr-, Be, U-, Th-, (W-) mineralisations in central and northern Nordland are presented. The investigated and sampled mineralisations were proposed in NGU report 2009.037 on the basis if existing reports and geochemical data sets. The investigation targets were evolved Proterozoic TIB-type granites (TIB = Trans-Scandinavian Igneous Belt) of the Tysfjord, Sommerset and Rishaugfjell basement windows, in particular, the Hatten- Tilthornet massif, Hundholmen, Kjerrfjellet, Hellemobotn, Reinoksskardet, upper Gjerdalen areas, the Sommerset basement Window, Rismålsvatn, and Memaurvatn. The general aim was to identify Zr-Ree mineralisations with >= 2wt.% REO (including Y2O3; REO - rare earth oxides) which are possibly enriched in Be, U and Th as well. |
Feltprøver |
Prøvenr. | Prøvetype | Diverse | |||||
23091001 | Fastfjell |
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23091002 | Fastfjell |
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23091003 | Fastfjell |
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23091004 | Fastfjell |
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28091009 | Fastfjell |
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NB! Alle analyseverdier er vist i slutten av utskriften.: |
Analyseresultater |
fra |
Forekomstområde 1845 - 014 Gjerdalsvann |
Elementanalyser |
( *=parts pr. million, #=parts pr.billion, Negative verdier betyr under deteksjonsgrensen.) |
Prøvenr. | Prøvetype | Cu* | Zn* | Pb* | Co* | Ni* | Au# | As* |
23091001 | Fastfjell | 0 | 74 | 6 | 1 | 1 | -.5 | 1 |
23091002 | Fastfjell | 0 | 59 | 8 | 1 | 0 | -.5 | 1 |
23091003 | Fastfjell | 1 | 72 | 10 | 1 | -0 | -.5 | 1 |
23091004 | Fastfjell | 0 | 53 | 8 | 1 | 1 | -.5 | 1 |
28091009 | Fastfjell | 0 | 38 | 3 | 1 | 0 | -.5 | -1 |
------------------ |
Prøvenr. | Cd* | Ba* | Mo* | Sn* | Sb* | Bi* | Se* | Ga* | V* |
23091001 | -.1 | 357 | 1.80 | 2 | -0 | -0 | -0.50 | 20.40 | -8 |
23091002 | -.1 | 341 | 2.40 | 2 | -0 | -0 | -0.50 | 20.30 | -8 |
23091003 | -.1 | 439 | 2.00 | 1 | -0 | -0 | -0.50 | 24.10 | -8 |
23091004 | -.1 | 261 | 0.40 | -1 | -0 | -0 | -0.50 | 19.80 | -8 |
28091009 | -.1 | 388 | 2.20 | 2 | -0 | -0 | -0.50 | 18.60 | -8 |
------------------ |
Prøvenr. | Th* | U* | W* | Rb* | Sr* | Y* | Zr* | Nb* | Cs* |
23091001 | 56.10 | 21.60 | -1 | 241.8 | 86.9 | 31.9 | 218 | 24.10 | 1.90 |
23091002 | 41.90 | 13.90 | -1 | 266.1 | 87.0 | 34.7 | 203 | 22.00 | 2.60 |
23091003 | 30.30 | 4.60 | -1 | 233.5 | 79.9 | 53.3 | 382 | 31.40 | 0.80 |
23091004 | 44.00 | 10.10 | -1 | 243.1 | 78.1 | 24.4 | 164 | 22.50 | 2.40 |
28091009 | 37.60 | 4.90 | -1 | 224.2 | 113.8 | 19.0 | 230 | 19.10 | 1.20 |
------------------ |
Prøvenr. | La* | Ce* | Pr* | Nd* | Sm* | Eu* | Gd* | Tb* | Dy* |
23091001 | 95.60 | 197.60 | 19.27 | 63.70 | 9.45 | 0.61 | 6.63 | 1.04 | 5.72 |
23091002 | 94.50 | 184.70 | 19.04 | 61.90 | 9.35 | 0.62 | 6.98 | 1.14 | 6.27 |
23091003 | 198.70 | 444.00 | 42.56 | 148.20 | 20.03 | 1.27 | 13.61 | 2.03 | 10.06 |
23091004 | 62.10 | 127.60 | 13.34 | 44.50 | 6.75 | 0.48 | 5.27 | 0.85 | 4.50 |
28091009 | 7.90 | 33.00 | 1.99 | 6.80 | 1.91 | 0.23 | 1.81 | 0.42 | 2.84 |
------------------ |
Prøvenr. | Ho* | Er* | Tm* | Yb* | Lu* | Be* | Hf* | Hg* | Tl* |
23091001 | 1.10 | 3.05 | 0.48 | 2.97 | 0.40 | 5 | 6.50 | -0 | 1 |
23091002 | 1.24 | 3.60 | 0.53 | 3.33 | 0.51 | 4 | 6.90 | -0 | 1 |
23091003 | 1.90 | 5.51 | 0.80 | 4.86 | 0.75 | 3 | 10.60 | -0 | 0 |
23091004 | 0.91 | 2.49 | 0.37 | 2.29 | 0.32 | 4 | 5.90 | -0 | 1 |
28091009 | 0.66 | 2.07 | 0.31 | 2.19 | 0.31 | 3 | 7.10 | -0 | 0 |
Oksydanalyser |
(Alle verdier er i %) |
Prøvenr. | Prøvetype | SiO2 | Al2O3 | TiO2 | Fe2O3 | MnO | MgO | CaO |
23091001 | Fastfjell | 73.72 | 13.61 | 0.22 | 2.09 | 0.03 | 0.27 | 0.77 |
23091002 | Fastfjell | 74.09 | 13.48 | 0.19 | 1.86 | 0.04 | 0.21 | 0.77 |
23091003 | Fastfjell | 73.32 | 13.08 | 0.23 | 2.49 | 0.05 | 0.08 | 0.77 |
23091004 | Fastfjell | 74.54 | 13.44 | 0.16 | 1.60 | 0.03 | 0.22 | 0.72 |
28091009 | Fastfjell | 73.20 | 13.68 | 0.19 | 1.90 | 0.04 | 0.21 | 0.97 |
------------------ |
Prøvenr. | Na2O | K2O | P2O5 | Loss | Sum | ||||
23091001 | 3.92 | 5.02 | 0.04 | 0.20 | 100.00 | ||||
23091002 | 3.65 | 5.27 | 0.04 | 0.30 | 100.00 | ||||
23091003 | 3.34 | 6.01 | 0.03 | 0.40 | 100.00 | ||||
23091004 | 3.96 | 4.93 | 0.03 | 0.30 | 100.00 | ||||
28091009 | 3.44 | 5.54 | 0.04 | 0.70 | 100.00 |
Faktaarket ble generert 22.11.2024 |
Spørsmål eller kommentarer vedrørende faktaarket kan mailes til: ressursdatabaser@ngu.no |
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