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MALMDATABASEN | |||||
Forekomstområde 1849 - 009 | |||||
(Sist oppdatert 23.okt.2024) |
Navn på forekomstområde : Hellemobotn |
(Objekt Id : 1849,009,00,00) |
Lokalisering |
Fylke : | Nordland (18) | Kommune : | Hamarøy (1849) |
Kart 1:50000: | Hellemobotn (2230-4) | Kart 1:250000: | Sulitjelma |
Markeringspunkt: | Lengdegrad: | 16.5771420 | Breddegrad: | 67.7914790 |
EU89-UTM Zone 33 | (Koordinatene ER bekreftet) |
X-koord: | 566519 m. | Y-koord: | 7520464 m. |
|
Materialtype |
Hovedtype: | Spesialmetaller (Nb,Ta,Be,Li,Sc,REE) | Subtype: | REE-metaller | |
Element(er): | Zr La CE Y Nb Yb |
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 |
Mûller (2011) gives the folloing description Romer et al. (1992) provided a geochemical data set from the Hellemobotn granite gneisses. Four of the analyses showed unusually high REE-Th-U concentrations (Müller 2010). The samples originated from Amásvágge, ca. 4 km SE of Hellemobotn and were collected by A. Korneliussen and T. Grenne (NGU) in 1988. Figure 30 shows the route and sampling locations of the author following the route of Korneliussen and Grenne. The area is characterised by a high variability of gneiss textures including fine-, medium- and coarsegrained and porphyritic varieties. The background gamma-ray intensity is relatively high for all granite varieties, ranging from 500 to 900 cps. The gamma-ray anomaly was identified at 33V 566560/7520281 (sample 25091004) exactly at the site where A. Korneliussen and T. Grenne took the samples with high REE concentrations (Fig. 30b). The mineralised granite gneiss forms a NNW-striking, dyke-like structure which is 30 m wide. Due to the limited time the dyke could be followed for 300 m but it is presumably much longer. The mineralisation comprises et least 600 000 t assuming a minimum length of 300 m, a width of 30 m and a vertical extension of about 25 m. The ground-measured anomaly coincides with a small airborne-measured Th-radiation anomaly (Fig. 31). The anomaly lies on a NNW-NW striking structure which extends from the Swedish border to Vuodnabattjåhkkå, interrupted by the Ávttje canyon (Fig. 31). Three samples (25091001 to -03) were collected from the high gamma-radiation area (>1000 cps) which forms a dyke-like structure consisting of medium-grained biotite granite gneiss. In addition, four different textural types of granite gneiss (samples 25091004 to -07) with gamma-ray signals from 500 - 900 cps were sampled (Fig. 30b). The highly radioactive samples contain 0.085 to 0.203 wt.% REO+Y2O3, the highest values reported in this project (Fig. 23). Zr concentrations range from 443 to 909 ppm, Th from 91 to 138 ppm and U from 20 to 33 ppm. The concentrations of the less radioactive granite gneisses are 0.018 to 0.038 wt.% REO+Y2O3, 185 to 383 ppm Zr, 23 to 70 ppm Th, 4 to 18 ppm U. In the case of the Hellemobotn granite gneisses, the gamma-ray radiation intensity correlates with REE-Th-U content. The highly radioactive samples are enriched in LREE and HREE compared to average granite (Fig. 32). Titanite is the most common accessory mineral in the highly radioactive samples, with grain sizes of 40 to 2000 µm (Fig. 33; Table 1). The REE concentrations of titanite are low, <1%, but it is, nevertheless, considered as an important carrier of the LREE because of the its high abundance. Th-rich allanite occurs as inclusions in titanite and it seems that titanite replaced allanite (Fig. 33a). Allanite is the major accessory mineral in the less radioactive samples. Other common accessories are zircon (20-160 µm), apatite (20-60 µm) and magnetite (40-1000 µm). Less common accessories are fluorite (20-200 µm), polycrase-(Y) (5-10 mm) and thorianite (5-10 µm). Sample 25091006 contains large ilmenite crystals with exsolution structures. |
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 | |||||
25091001 | Fastfjell |
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25091002 | Fastfjell |
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25091003 | Fastfjell |
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25091004 | Fastfjell |
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25091005 | Fastfjell |
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25091006 | Fastfjell |
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25091007 | Fastfjell |
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NB! Alle analyseverdier er vist i slutten av utskriften.: |
Analyseresultater |
fra |
Forekomstområde 1849 - 009 Hellemobotn |
Elementanalyser |
( *=parts pr. million, #=parts pr.billion, Negative verdier betyr under deteksjonsgrensen.) |
Prøvenr. | Prøvetype | Cu* | Zn* | Pb* | Co* | Ni* | Au# | As* |
25091001 | Fastfjell | -0 | 86 | 9 | 3 | 0 | -.5 | 1 |
25091002 | Fastfjell | 0 | 103 | 11 | 4 | 1 | -.5 | 2 |
25091003 | Fastfjell | 0 | 143 | 10 | 5 | 1 | -.5 | 2 |
25091004 | Fastfjell | 0 | 51 | 7 | 2 | 0 | -.5 | 1 |
25091005 | Fastfjell | 1 | 43 | 4 | 3 | 1 | -.5 | 1 |
25091006 | Fastfjell | 0 | 15 | 4 | 3 | 1 | -.5 | -1 |
25091007 | Fastfjell | 3 | 27 | 8 | 1 | 0 | -.5 | -1 |
------------------ |
Prøvenr. | Cd* | Ba* | Mo* | Sn* | Sb* | Bi* | Se* | Ga* | V* |
25091001 | -.1 | 246 | 0.70 | 4 | -0 | -0 | -0.50 | 25.20 | 8 |
25091002 | -.1 | 190 | 1.50 | 5 | -0 | -0 | -0.50 | 26.20 | 12 |
25091003 | -.1 | 166 | 1.60 | 8 | -0 | -0 | -0.50 | 27.20 | 16 |
25091004 | -.1 | 229 | 3.20 | 2 | -0 | -0 | -0.50 | 22.20 | -8 |
25091005 | -.1 | 756 | 2.60 | 2 | -0 | -0 | -0.50 | 21.00 | 21 |
25091006 | -.1 | 137 | -0.10 | 4 | -0 | 0 | -0.50 | 21.50 | -8 |
25091007 | -.1 | 186 | 0.10 | 3 | -0 | -0 | -0.50 | 20.80 | -8 |
------------------ |
Prøvenr. | Th* | U* | W* | Rb* | Sr* | Y* | Zr* | Nb* | Cs* |
25091001 | 90.80 | 20.20 | -1 | 292.5 | 80.6 | 51.0 | 443 | 30.20 | 3.10 |
25091002 | 121.80 | 29.30 | 1 | 261.4 | 78.3 | 93.1 | 684 | 42.10 | 3.10 |
25091003 | 137.70 | 33.40 | -1 | 299.1 | 63.0 | 117.5 | 910 | 59.90 | 4.80 |
25091004 | 70.00 | 17.60 | 1 | 288.4 | 70.0 | 38.3 | 311 | 21.60 | 2.30 |
25091005 | 23.10 | 3.80 | -1 | 229.9 | 154.0 | 24.2 | 383 | 19.40 | 1.30 |
25091006 | 62.60 | 13.60 | 1 | 270.0 | 89.7 | 29.3 | 185 | 23.50 | 0.90 |
25091007 | 58.20 | 15.80 | -1 | 303.5 | 48.7 | 36.7 | 210 | 22.40 | 1.30 |
------------------ |
Prøvenr. | La* | Ce* | Pr* | Nd* | Sm* | Eu* | Gd* | Tb* | Dy* |
25091001 | 161.10 | 332.50 | 31.21 | 99.30 | 14.58 | 0.60 | 9.83 | 1.58 | 9.25 |
25091002 | 322.50 | 640.50 | 58.08 | 189.00 | 25.68 | 0.77 | 18.17 | 2.82 | 15.77 |
25091003 | 398.80 | 791.40 | 72.96 | 233.20 | 31.88 | 0.76 | 22.50 | 3.64 | 19.83 |
25091004 | 121.60 | 259.00 | 24.58 | 80.10 | 12.01 | 0.62 | 7.75 | 1.24 | 6.71 |
25091005 | 69.10 | 161.70 | 15.52 | 52.00 | 8.03 | 0.80 | 5.50 | 0.84 | 4.40 |
25091006 | 26.90 | 71.70 | 6.03 | 19.50 | 3.34 | 0.20 | 2.62 | 0.57 | 3.75 |
25091007 | 60.80 | 133.00 | 12.54 | 40.90 | 6.89 | 0.33 | 5.44 | 0.95 | 5.57 |
------------------ |
Prøvenr. | Ho* | Er* | Tm* | Yb* | Lu* | Be* | Hf* | Hg* | Tl* |
25091001 | 1.68 | 5.05 | 0.76 | 5.14 | 0.77 | 7 | 12.40 | -0 | 1 |
25091002 | 2.97 | 8.60 | 1.29 | 8.32 | 1.26 | 6 | 18.70 | -0 | 1 |
25091003 | 3.89 | 11.48 | 1.75 | 11.34 | 1.72 | 7 | 26.30 | -0 | 2 |
25091004 | 1.22 | 3.64 | 0.55 | 3.54 | 0.52 | 5 | 10.30 | -0 | 1 |
25091005 | 0.82 | 2.28 | 0.33 | 2.12 | 0.32 | 4 | 10.00 | -0 | 1 |
25091006 | 0.89 | 2.93 | 0.49 | 3.21 | 0.47 | 5 | 7.40 | -0 | 0 |
25091007 | 1.13 | 3.55 | 0.59 | 4.04 | 0.62 | 5 | 7.30 | -0 | 0 |
Oksydanalyser |
(Alle verdier er i %) |
Prøvenr. | Prøvetype | SiO2 | Al2O3 | TiO2 | Fe2O3 | MnO | MgO | CaO |
25091001 | Fastfjell | 69.29 | 14.77 | 0.41 | 3.42 | 0.06 | 0.43 | 1.20 |
25091002 | Fastfjell | 69.39 | 13.51 | 0.55 | 4.92 | 0.09 | 0.65 | 1.47 |
25091003 | Fastfjell | 68.86 | 12.61 | 0.76 | 6.43 | 0.11 | 0.72 | 1.75 |
25091004 | Fastfjell | 71.82 | 14.58 | 0.24 | 2.26 | 0.04 | 0.32 | 0.88 |
25091005 | Fastfjell | 70.92 | 14.05 | 0.37 | 2.78 | 0.04 | 0.37 | 1.28 |
25091006 | Fastfjell | 76.12 | 12.56 | 0.15 | 1.44 | 0.02 | 0.24 | 0.48 |
25091007 | Fastfjell | 74.97 | 12.70 | 0.18 | 1.81 | 0.04 | 0.17 | 0.80 |
------------------ |
Prøvenr. | Na2O | K2O | P2O5 | Loss | Sum | ||||
25091001 | 4.05 | 5.42 | 0.07 | 0.70 | 100.00 | ||||
25091002 | 3.84 | 4.33 | 0.10 | 0.80 | 100.00 | ||||
25091003 | 3.53 | 3.89 | 0.15 | 0.80 | 100.00 | ||||
25091004 | 4.12 | 5.27 | 0.04 | 0.30 | 100.00 | ||||
25091005 | 3.66 | 5.51 | 0.08 | 0.80 | 100.00 | ||||
25091006 | 3.65 | 4.77 | 0.03 | 0.50 | 100.00 | ||||
25091007 | 3.52 | 5.30 | 0.04 | 0.40 | 100.00 |
Faktaarket ble generert 22.11.2024 |
Spørsmål eller kommentarer vedrørende faktaarket kan mailes til: ressursdatabaser@ngu.no |
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