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THE ORE DATABASE
Deposit Area 1845 - 013
(Last updated 23.okt.2024)

Name of Deposit Area : Memaurvann
(Object Id : 1845,013,00,00)

Location
County : Nordland (18) Municipality : Sørfold (1845)
Map 1:50000: Fauske (2129-4) Map 1:250000: Sulitjelma
Marking point: Longitude: 15.6806400 Latitude: 67.3637940
EU89-UTM Zone 33 (Coordinates IS confirmed)
X-coord: 529233 m. Y-coord: 7472096 m.

Commodity
Main Type: Special metals (Nb,Ta,Be,Li,Sc,REE) Sub Type: REE-metals
Element(s): Zr La Y CE
Production
Activity: Exploration Reserves:
Prod. method: Production:
Prod. status: Volume of dump:

Importance
Public: (No data)
Economical: Could be significant , (Confirmed 22.okt.2024 by Havard Gautneb)

Mineralization
Era: Period:
Dating: Method:
Genesis: Form:
Main texture: Min. distribution:
Main grain size: Main alteration:
Strike/Dip: Direction:
Plunge:
Stratigraphic classification of host rock
Era: Period:
Province:
Geotec.unit:
Tectonic complex:
Igneous complex:
Group: Formation:

Information(s) in free text format
Free text
Müller 2011 refport the following regarding the Memaurvann occurrence The reason for sampling the granite gneiss of the northern Rishaugfjell window was one Uranal database analysis of a TIB-granite sample from Memaurvatn (UTM 33W 529233E/7472096N) which contained 11700 ppm Zr and 884 ppm Y+La+Ce. During the field campaign two areas of coarse-grained biotite granite gneiss (ca. 130 x 30 m and 150 x 5 m) with high gamma radiation (>1000 cps) were identified south of the lake Memaurvatn The estimated resource is about 300 000 tons assuming a vertical extension of the mineralisation of 25 m. The mineralised granite gneiss contains aggregates of fine-grained violet fluorite with crystal sizes of up to 1 mm. The gamma radiation of the nonmineralised, fluorite-free host granite gneiss is about 480 cps. Three samples were collected: two mineralized coarse-grained biotite granite gneisses (samples 22091002 and 22091003) and one non-mineralised coarse-grained biotite granite gneiss (sample 22091001). All three samples have REO concentrations of 0.064 to 0.070 wt.% REO (Fig. 8). Sample 22091001 is characterized by high Zr - 1658 ppm and high U - 134 ppm (Appendix 2). The REE distribution pattern indicates that LREE and HREE are enriched in samples 22091001 and 22091002 compared to average granite composition according to Turekian and Wedepohl (1961) (Fig. 9). In addition, the Memaurvatn granite gneiss is characterized by a strong Eu anomaly indicating a strong fractional crystallization. The fluorite-bearing sample 22091003 is slightly depleted in HREE. It is assumed, that the fluorite-forming fluids caused the HREE depletion in sample 22091003. Thus, high gammaray signals measured with the scintillometer in the field do not necessarily detect all rocks with elevated REE-Zr concentrations. SEM investigations revealed that allanite and zircon are the most common accessory REE-bearing minerals (Fig. 10, Table 1). Fluorite is particularly common in sample 22091003 but it contains <1 % REE. Apatite, monazite or xenotime, which are common accessories in granitic rocks, could not be identified. Allanite crystals are 40 to 120 µm in size and carry most of the LREE. Zircon forms two generations: an older, porous, partially dissolved generation, with grain sizes of 20 to 80 µm and younger, euhedral, homogeneous generations with grain sizes of 5 to 10 µm. Zircon is the major carrier of the HREE. In addition there are some titanite crystals, 10 to 50 µm. In sample 22091003 zircons of generation 1 are most intensely dissolved which explains the depletion of HREE. Titanite can be an important carrier of LREE (e.g. Seifert 2005) but EDX analysis revealed that the REE content of the titanites is <1 wt.%.

Bibliography:
From NGU's Reference Archive:
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 pages
Abstract:
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.

Fieldsamples
Sample No. Sample type Miscellanrous
22091001 Bedrock
Sampler :Axel M¿ller
Comment :coarse-grained biotite granite gneiss, non-mineralised, UTM east 528891, UTM north 7472316
No. of registrated element analyses = 1
No. of registrated oxide analyses = 1
22091002 Bedrock
Sampler :Axel M¿ller
Comment :coarse-grained biotite granite gneiss, mineralised, UTM east 529262, UTM north 7472074
No. of registrated element analyses = 1
No. of registrated oxide analyses = 1
22091003 Bedrock
Sampler :Axel M¿ller
Comment :coarse-grained biotite granite gneiss with fluorite, mineralised, UTM east 529191, UTM north 7471937
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 1845 - 013 Memaurvann

Element analyses

( *=parts pr. million, #=parts pr.billion, Negative values means below detection limit value.)
Sample No. Sample Type Cu* Zn* Pb* Co* Ni* Au# As*
22091001 Bedrock 2 67 7 1 1 -.5 6
22091002 Bedrock 2 89 13 2 4 -.5 4
22091003 Bedrock 6 37 22 1 1 -.5 10
------------------
Sample No. Cd* Ba* Mo* Sn* Sb* Bi* Se* Ga* V*
22091001 -.1 405 0.20 6 1 0 1.20 24.80 -8
22091002 .4 279 0.30 6 0 0 2.20 23.70 -8
22091003 -.1 137 4.50 3 1 0 1.20 24.60 -8
------------------
Sample No. Th* U* W* Rb* Sr* Y* Zr* Nb* Cs*
22091001 41.10 12.70 1 286.1 75.9 65.1 541 33.70 3.50
22091002 35.10 134.50 1 292.7 58.8 158.3 1658 28.80 4.70
22091003 61.50 10.10 1 314.3 31.2 30.7 113 18.80 2.90
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Sample No. La* Ce* Pr* Nd* Sm* Eu* Gd* Tb* Dy*
22091001 107.40 241.80 25.99 94.50 15.81 1.00 12.02 2.11 12.01
22091002 74.20 161.40 17.32 60.30 14.76 0.82 17.34 2.94 18.95
22091003 125.40 268.00 22.52 70.50 9.34 0.44 4.96 0.90 4.89
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Sample No. Ho* Er* Tm* Yb* Lu* Be* Hf* Hg* Tl*
22091001 2.39 6.61 0.97 6.47 0.96 8 15.80 -0 1
22091002 4.30 13.05 1.79 11.04 1.59 8 29.90 -0 1
22091003 0.96 2.92 0.46 3.36 0.53 8 4.50 -0 0

Oxide analyses

( All values are in % )
Sample No. Sample Type SiO2 Al2O3 TiO2 Fe2O3 MnO MgO CaO
22091001 Bedrock 72.06 13.23 0.34 3.39 0.05 0.41 0.80
22091002 Bedrock 72.56 12.43 0.27 3.93 0.08 0.62 0.58
22091003 Bedrock 74.60 12.72 0.10 1.66 0.02 0.11 0.75
------------------
Sample No. Na2O K2O P2O5 Loss Sum
22091001 3.37 5.72 0.05 0.40 100.00
22091002 3.03 5.63 0.04 0.50 100.00
22091003 3.39 5.94 0.02 0.60 100.00


The fact sheet was created on 22.11.2024

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