Norsk versjon | |||||
THE ORE DATABASE | |||||
Occurence 5027 - 013 Fløttum | |||||
(Object Id: 4439) (Last updated: 07.11.2023) |
Drill Cores: Fløttum |
|
Location |
County: | Trøndelag | Municipality: | Midtre Gauldal (5027) |
Map 1:50000: | Haltdalen (1620-1) | Map 1:250000: | Røros |
Coordinate system: | EU89-UTM Zone 32 |
East: | 587394 m. | North: | 6975451 m. |
Longitude: | 10.7195490 | Latitude: | 62.8985320 |
Show on map |
|
Resource |
Resource Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Resource Subtype: | Zinc | |
Element(s): | Zn Cu Kis |
Importance |
Raw material meaning: | Not Assessed (reg. 20.03.2017) |
Resources and production |
Activity: | Test mining | Reserves: | 350 thousand tons | |
Operating method: | Underground mining | Historical production: |
Products |
Element/product | Crude ore grade or quality | Reg. date | |
Ag | 29 ppm | 18.10.2012 | |
Cu | 0,96 % | 18.10.2012 | |
Zn | 4,76 % | 18.10.2012 |
Operations |
From - To | Activity | Comments | |
1888 - 1892 | Test mining | Company/Institution :Røros Kobberverk | |
1890 - 1891 | Core drilling | Company/Institution :Røros Kobberverk | |
1904 - 1910 | Test mining | Company/Institution :Røros Kobberverk | |
1913 - 1913 | Core drilling | Company/Institution :Røros Kobberverk | |
1915 - 1917 | Test mining | Company/Institution :Røros Kobberverk | |
1949 - 1949 | Geophysics | Company/Institution :Geofysisk Malmleting | |
1952 - 1953 | Core drilling | Company/Institution :Røros Kobberverk | |
1953 - 1953 | Geology | Company/Institution :Ljøkjell, dipl. NTH | |
1970 - 1971 | Geophysics | Company/Institution :Røros Kobberverk/Terratest A/S | |
1974 - 1974 | Geochemistry | Company/Institution :Røros Kobberverk/Sydvaranger | |
1974 - 1974 | Geophysics | Company/Institution :Røros Kobberverk/Sydvaranger | |
1997 - 1997 | Sampling | Company/Institution :NGU-Malmreg. |
Mineralization |
Era: | Paleozoic | Period: | ||
Genesis: | Volcex | Form: | Layer | |
Main texture: | Banded | Min. distribution: | Massive (>50 % ore minerals) |
Main grain size: | Medium grained (1-3 mm) | Main alteration: | Silicification |
Strike/Dip: | 110 / 30 | Direction: | 150 | |
Plunge: | 30 |
Stratigraphic classification of host rock |
Era: | Paleozoic | Period: |
Province: | Caledonides | |
Geotec.unit: | Trondheim Nappe Complex | |
Tectonic complex: | Gula Nappe | |
Igneous complex: |
Group: | Gula | Formation: | Singsås |
Mineralogy |
Relationship | Mineral | Amount | |
Gangue mineral | Muscovite | Major mineral (>10%) | |
Gangue mineral | Quartz | Major mineral (>10%) | |
Gangue mineral | Sericite | Subordinate mineral (1-10%) | |
Gangue mineral | Feldspar | Subordinate mineral (1-10%) | |
Gangue mineral | Graphite | Subordinate mineral (1-10%) | |
Ore mineral | Pyrite | Major mineral (>10%) | |
Ore mineral | Chalcopyrite | Major mineral (>10%) | |
Ore mineral | Pyrrhotite | Major mineral (>10%) | |
Ore mineral | Sphalerite | Major mineral (>10%) | |
Ore mineral | Galena | Subordinate mineral (1-10%) | |
Ore mineral | Pyrargyrite | Accessory mineral (<1%) | |
Ore mineral | Alabandite | Accessory mineral (<1%) | |
Ore mineral | Hessite | Accessory mineral (<1%) | |
Ore mineral | Molybdenite | Accessory mineral (<1%) | |
Ore mineral | Bismuth | Accessory mineral (<1%) | |
Ore mineral | Stannite | Accessory mineral (<1%) | |
Ore mineral | Tetrahedrite | Accessory mineral (<1%) | |
Ore mineral | Arsenopyrite | Accessory mineral (<1%) | |
Ore mineral | Mackinawite | Accessory mineral (<1%) |
Lithology: |
Relationship | Rock | Origin | |
Wall rock | Glimmerskifer | Sedimentary Original rock :Greywacke |
|
Metamorphic facies :Amphibolite | |||
Wall rock | Kvartsitt | Sedimentary | |
Metamorphic facies :Amphibolite | |||
Wall rock | Grafittskifer | Sedimentary | |
Metamorphic facies :Amphibolite |
Structures |
Location: | Type: | Orientation(360 gr.): | Relation to min.: | |
Host rock | Foliation | Strike/Dip :110 / 30 | Post-mineralisation ;...Effect :None | |
Host rock | Fold axis | Dir./Plunge :150 / 30 | Post-mineralisation ;...Effect :Modifies |
Information(s) in free text format |
Free text |
The Fløttum Cu-Zn deposit is associated with black banded quartzite and carbonaceous phyllite. The deposit consists of four inclined and ruler-shaped ore lenses, which perhaps originally were parts of one body, but later were disrupted by folding. The sulphides are pyrite, pyrrhotite, sphalerite, chalcopyrite and accessory galena. Close to the ore lenses, there are glassy muscovite-bearing quartzitic schists, most likely formed by hydrothermal processes during ore formation. During exploration, a dipartite division was established with a footwall and a hanging-wall ore type. The hanging wall ore consists of pyrite and subordinate sphalerite, whereas the footwall ore consists of pyrrhotite, sphalerite, chalcopyrite, galena, fahlore and arsenopyrite. Total possible ore reserves are estimated to 350,000 t with 0.96 % Cu, 4.76 % Zn and 29 ppm Ag. The deposit has only been subject to test mining. |
Bibliography: |
From NGU's Reference Archive: |
Gullichsen; Getz; Dalseth; Kvalheim , 1916 |
Fløttum Gruver. |
;Norges geologiske undersøkelse;FAGRAPPORT;Bergarkivet; No.BA 706;17 pages |
Bøckman, K.L. , 1938 |
Fløttum gruve. |
;Norges geologiske undersøkelse;FAGRAPPORT;Bergarkivet; No.BA 705;5 pages |
Abstract: | |
Rapporten er en uttalelse til styret for Røros Kobberverk. Rapporten er en gjennomgåelse av årsberetninger fra gruben fra 1888-1892 og 1904-1917. Det foreslås over for styret, på grunnlag av det framlagte materialet at det innledes forhandlinger med intresserte parter om håndgivelse av Fløttum grube for salg eller bortleie mot royalty. |
Holmsen, P. , 1939 |
Fløttum Gruver. |
;Norges geologiske undersøkelse;FAGRAPPORT;Bergarkivet; No.BA 707;5 pages |
Abstract: | |
Det er gjort vurdering av Røros kobberverks materiale angående gruben. Det påpekes at det må være et interessant grubeprosjekt. Oppfart malmkvantum er sikkert 150 000 tonn. Malmen har gull og sølvholdig arsenkis, sinkblende og nyrer av sølvholdig blyglans. Det kan bli snakk om utvinning av følgende mineralkonsentrat: Blykonsentrat med et visst innhold av sølv. Kobberkons. med sølv. Sinkkonsentrat med sølv, svovelkiskonsentrat og arsenkiskonsentrat med et visst gullinnhold. Malmen er meget kompleks og setter de største krav til oppredningsteknikken. Rapporten har også analyseresultat og tabeller fra flotasjonstester. |
Nilsen, Odd , 1978 |
Caledonian sulphide deposits and minor iron-formations from the southern Trondheim region, Norway. |
;Norges geologiske undersøkelse;TIDSSKRIFTARTIKKEL;NGU; No.340;35-85 + k pages |
Abstract: | |
Within the southern and central parts of the Trondheim region of the Norwegian Caledonides a great number of small, stratabound cupriferous pyrite deposits are confined to mafic metavolcanics of the Gula, Støren and Fundsjø Groups of the Lower Palaeozoic succession. The deposits occuring within, or in close contact with the metavolcanics are characterized by their association with minor manganiferous oxide/silicate iron-formations - better known as "vasskis" ore type - within the metamorphic low-grade areas. The iron-fprmations of the metamorphic higher grade terrains on the other hand, which are extensively developed within the Gula Group, are mostly of a pyrrhotitic sulphide/silicate type and sulphurization processes are thought to have played an important role during the metamorphism. The pyrite deposits occurring adjacent to the metavolcanics bear no relationship to the iron-formations. They are embedded in pelitic, often carbonaceous assemblages (Gula Group) or within tuffitic members of the volcanogene Støren Group, and they are thought to represent re-sedimented (reworked) deposits. The pyrite deposits display varying degree of metamorphic reconstitution and a tectonic control has apparently determined their disc- or ruler-shaped morphology. |
References not to be found in NGU's Reference Archive.: |
Pettersen, Ø. 1971: Rapport over malmletingsarbeider 1970. BV 50A-C. |
Gvein, Ø. 1990: Fløttumforekomsten i Midtre Gauldal, Sør-Trøndelag. Prospektering A/S rapp. nr. 2164. (BV 4143). |
Juhava, R. 1991: Fløttum forekomst - et tolkningsforslag. BV 4150. |
Ljøkjell, P. 1953: Fløttum gruve. Upubl. dipl.oppg. NTH. |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||
JS-G1902 | Dump |
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JS-G1903 | Dump |
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ST0237.TGST93.058 | Dump |
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ST0237.TGST93.059 | Dump |
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ST0237.TGST93.060 | Dump |
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ST0237.TGST93.061 | Dump |
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ST0237.01 | Dump |
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ST0237.02 | Dump |
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ST0237.03 | Dump |
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ST0237.04 | Dump |
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ST0237.05 | Dump |
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ST0237.06 | Dump |
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ST0237.07 | Dump |
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400011 | Dump |
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400012 | Dump |
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400013 | Dump |
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400014 | Dump |
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400015 | Dump |
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400016 | Dump |
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400017 | Dump |
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400018 | Dump |
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NB! All analyse values are shown at the end of the printout.: |
Name of Locality: |
(Object Id: 10108 13,01,00) |
|
Location |
County: | Trøndelag | Municipality: | Midtre Gauldal (5027) |
Map 1:50000: | Haltdalen (1620-1) | Map 1:250000: | Røros |
Coordinate system: | EU89-UTM Zone 32 |
East: | 587316 m. | North: | 6975589 m. |
Longitude: | 10.7180870 | Latitude: | 62.8997850 |
Show on map |
|
Resource |
Resource Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Resource Subtype: | Zinc | |
Element(s): | Zn Cu Kis |
Resources and production |
Activity: | Mining | Reserves: | ||
Operating method: | Underground mining | Historical production: |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||
JS-G1904 | Dump |
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JS-G1905 | Dump |
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JS-G1906 | Dump |
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JS-G1907 | Dump |
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JS-G1908 | Dump |
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JS-G1909 | Dump |
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NB! All analyse values are shown at the end of the printout.: |
Analyse Results |
from |
Deposit Area 5027 - 013 Fløttum |
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# |
JS-G1902 | Dump | 5130 | 195000 | 2430 | 38 | 46 | 42.4 | 79.0 |
JS-G1903 | Dump | 1395 | 137000 | 653 | 139 | 19 | 12.7 | 81.0 |
JS-G1904 | Dump | 59700 | 44100 | 3500 | 14 | 27 | 163.0 | 1190.0 |
JS-G1905 | Dump | 17500 | 158000 | 3350 | 16 | 56 | 48.6 | 69.0 |
JS-G1906 | Dump | 8950 | 70500 | 537 | 9 | 53 | 15.5 | 34.0 |
JS-G1907 | Dump | 95600 | 91500 | 2100 | 110 | 17 | 148.0 | 196.0 |
JS-G1908 | Dump | 193 | 3350 | 57 | 75 | 11 | 1.9 | 17.0 |
JS-G1909 | Dump | 2840 | 21600 | 82 | 37 | 53 | 5.6 | 25.0 |
ST0237.TGST93.058 | Dump | 9149 | 86488 | 3672 | 101 | 21 | 56.3 | 53.0 |
ST0237.TGST93.059 | Dump | 29600 | 97394 | 2198 | 7 | 58 | 40.5 | 56.0 |
ST0237.TGST93.060 | Dump | 2937 | 99999 | 13955 | 28 | 8 | 169.0 | 580.0 |
ST0237.TGST93.061 | Dump | 1922 | 39751 | 61 | 44 | 3 | 6.0 | 48.0 |
ST0237.01 | Dump | 29212 | 81796 | 2318 | 6 | 57 | 43.3 | 94.0 |
ST0237.02 | Dump | 99999 | 20603 | 150 | 105 | 19 | 175.8 | 951.0 |
ST0237.03 | Dump | 33608 | 95348 | 2042 | 104 | 38 | 61.0 | 397.0 |
ST0237.04 | Dump | 5424 | 99999 | 155 | 42 | 5 | 6.0 | 16.0 |
ST0237.05 | Dump | 1055 | 99999 | 228 | 17 | 4 | -.3 | 17.0 |
ST0237.06 | Dump | 6321 | 17952 | 704 | 137 | 45 | 19.0 | 108.0 |
ST0237.07 | Dump | -1 | 99999 | 2059 | 44 | 7 | 5.7 | 32.0 |
400011 | Dump | 78500 | 101300 | 997 | 99 | 19 | 56.9 | 409.0 |
400012 | Dump | 6567 | 147700 | 110 | 154 | 22 | 6.4 | 64.0 |
400013 | Dump | 12000 | 112400 | 3749 | 204 | 20 | 28.8 | 97.0 |
400014 | Dump | 874 | 329500 | 2934 | 19 | 8 | 15.1 | 87.0 |
400015 | Dump | 26600 | 6060 | 795 | 30 | 11 | 27.9 | 450.0 |
400016 | Dump | 18900 | 99000 | 194 | 18 | 38 | 7.4 | 110.0 |
400017 | Dump | 16600 | 213400 | 342 | 13 | 34 | 17.4 | 142.0 |
400018 | Dump | 762 | 287000 | 3652 | 36 | 12 | 32.4 | 96.0 |
------------------ |
Sample No. | Pt# | Pd# | As* | Cd* | Ba* | Mo* | Sn* | Sb* | Bi* |
JS-G1902 | -5.0 | -1.0 | 30 | 650.0 | 10 | 41.10 | 13 | 7 | 75 |
JS-G1903 | -5.0 | 2.0 | 387 | 409.0 | 30 | 79.60 | 20 | 6 | 10 |
JS-G1904 | -5.0 | 5.0 | 1130 | 135.5 | 60 | 38.50 | 119 | 45 | 121 |
JS-G1905 | -5.0 | 1.0 | 47 | 338.0 | -10 | 43.80 | 63 | 7 | 74 |
JS-G1906 | -5.0 | 1.0 | 5 | 179.0 | 10 | 21.20 | 25 | 4 | 17 |
JS-G1907 | -5.0 | 2.0 | 508 | 289.0 | 30 | 47.50 | 53 | 17 | 37 |
JS-G1908 | -5.0 | -1.0 | 354 | 9.5 | 10 | 39.30 | 8 | 1 | 1 |
JS-G1909 | -5.0 | 3.0 | 30 | 54.6 | 10 | 16.15 | 3 | 2 | 8 |
ST0237.TGST93.058 | 232 | 213.5 | -1 | 38.00 | 8 | 83 | |||
ST0237.TGST93.059 | 8 | 191.0 | -1 | 21.00 | 2 | 87 | |||
ST0237.TGST93.060 | 173 | 675.1 | 5 | 84.00 | 25 | 301 | |||
ST0237.TGST93.061 | 264 | 81.4 | -1 | 6.00 | -2 | -2 | |||
ST0237.01 | -1.0 | -1.0 | 2 | 227.1 | 4 | 25.00 | -3 | 84 | |
ST0237.02 | 1.0 | -1.0 | 581 | 88.1 | 13 | 12.00 | 53 | 24 | |
ST0237.03 | 3.0 | -1.0 | 259 | 231.0 | -1 | 16.00 | 16 | 58 | |
ST0237.04 | 1.0 | -1.0 | 193 | 343.8 | -1 | 10.00 | -3 | 13 | |
ST0237.05 | -1.0 | 1.0 | 169 | 739.7 | 4 | 3.00 | -3 | 9 | |
ST0237.06 | 6.0 | 10.0 | 98 | 62.4 | 7 | 2.00 | -3 | 37 | |
ST0237.07 | 1.0 | -1.0 | 175 | 1201.0 | 4 | 4.00 | -3 | 32 | |
400011 | 286 | 252.8 | 3 | 33.00 | 11 | 16 | |||
400012 | 304 | 351.9 | 3 | 36.00 | 3 | 3 | |||
400013 | 264 | 176.7 | 16 | 10.00 | 10 | 89 | |||
400014 | 31 | 877.4 | 13 | 122.00 | 3 | 107 | |||
400015 | 133 | 27.9 | 37 | 13.00 | 9 | 13 | |||
400016 | 40 | 184.8 | 1 | 7.00 | 5 | 6 | |||
400017 | 166 | 347.5 | 2 | 13.00 | 6 | 10 | |||
400018 | 172 | 677.4 | 7 | 154.00 | 8 | 49 |
------------------ |
Sample No. | Se* | Ga* | Ge* | In* | S% | V* | Cr* | Mn* | Fe% |
JS-G1902 | 22.00 | 28.90 | 0.36 | 19.60 | 10.00 | 21 | 8 | 1620 | 24.60 |
JS-G1903 | 50.00 | 30.40 | 0.50 | 11.80 | 10.00 | 33 | 5 | 800 | 26.30 |
JS-G1904 | 82.00 | 32.20 | 0.30 | 12.10 | 10.00 | 32 | 6 | 876 | 20.40 |
JS-G1905 | 52.00 | 22.30 | 0.52 | 5.04 | 10.00 | 25 | 4 | 1640 | 32.10 |
JS-G1906 | 56.00 | 10.60 | 0.64 | 5.87 | 10.00 | 19 | 6 | 935 | 41.70 |
JS-G1907 | 56.00 | 24.80 | 0.52 | 5.97 | 10.00 | 14 | 5 | 679 | 28.70 |
JS-G1908 | 32.00 | 0.99 | 0.09 | 0.71 | 10.00 | 3 | 5 | 141 | 29.20 |
JS-G1909 | 62.00 | 5.42 | 0.54 | 6.01 | 10.00 | 9 | 8 | 482 | 34.00 |
ST0237.TGST93.058 | 15 | 3 | 712 | 26.92 | |||||
ST0237.TGST93.059 | 13 | -1 | 1435 | 32.51 | |||||
ST0237.TGST93.060 | 27 | 8 | 1051 | 9.24 | |||||
ST0237.TGST93.061 | 1 | -1 | 332 | 22.61 | |||||
ST0237.01 | 27.80 | 13 | 2 | 1589 | 44.12 | ||||
ST0237.02 | 27.30 | 9 | -1 | 446 | 32.88 | ||||
ST0237.03 | 30.70 | 14 | 5 | 805 | 40.82 | ||||
ST0237.04 | 44.50 | 11 | 11 | 775 | 18.40 | ||||
ST0237.05 | 36.10 | 5 | 9 | 1433 | 16.47 | ||||
ST0237.06 | 34.70 | 15 | 3 | 298 | 47.12 | ||||
ST0237.07 | 36.00 | 4 | 10 | 1361 | 16.87 | ||||
400011 | 13 | 38 | 726 | 10.00 | |||||
400012 | 17 | 78 | 955 | 29.35 | |||||
400013 | 17 | 72 | 463 | 38.57 | |||||
400014 | 12 | 110 | 2305 | 6.17 | |||||
400015 | 26 | 86 | 183 | 8.77 | |||||
400016 | 16 | 36 | 904 | 10.00 | |||||
400017 | 23 | 19 | 1272 | 10.00 | |||||
400018 | 14 | 59 | 825 | 10.00 |
------------------ |
Sample No. | Th* | U* | W* | Rb* | Sr* | Y* | Zr* | Nb* | Ta* |
JS-G1902 | 0.21 | 1.30 | 1 | 3.5 | 36.3 | 5.4 | 9 | 0.20 | -0.05 |
JS-G1903 | 0.19 | 1.70 | 3 | 10.8 | 22.5 | 5.6 | 13 | 0.20 | -0.05 |
JS-G1904 | 1.16 | 1.70 | 3 | 27.6 | 44.8 | 15.7 | 93 | 1.50 | 0.13 |
JS-G1905 | 0.05 | 0.40 | 2 | 0.3 | 1.2 | 0.9 | 1 | 0.10 | -0.05 |
JS-G1906 | 0.05 | 0.60 | 2 | 0.6 | 4.5 | 0.9 | 1 | 0.10 | -0.05 |
JS-G1907 | 0.28 | 0.90 | 3 | 6.0 | 6.9 | 3.4 | 4 | 0.20 | -0.05 |
JS-G1908 | 0.07 | 0.30 | 1 | 0.5 | 3.4 | 0.5 | 3 | 0.20 | -0.05 |
JS-G1909 | 0.06 | 0.10 | 1 | 0.7 | 0.8 | 0.4 | 2 | 0.10 | -0.05 |
ST0237.TGST93.058 | 2.00 | -5.00 | -2 | 12.0 | |||||
ST0237.TGST93.059 | 2.00 | -5.00 | -2 | 1.0 | |||||
ST0237.TGST93.060 | 2.00 | 7.00 | 5 | 26.0 | |||||
ST0237.TGST93.061 | -2.00 | 5.00 | -2 | 8.0 | |||||
ST0237.01 | 6.00 | -8.00 | -2 | 3.0 | |||||
ST0237.02 | 5.00 | -8.00 | -2 | 2.0 | |||||
ST0237.03 | 6.00 | -8.00 | -2 | 1.0 | |||||
ST0237.04 | 4.00 | -8.00 | -2 | 1.0 | |||||
ST0237.05 | 2.00 | -8.00 | -2 | 19.0 | |||||
ST0237.06 | 8.00 | -8.00 | -2 | 1.0 | |||||
ST0237.07 | 4.00 | -8.00 | -2 | 16.0 | |||||
400011 | 6.0 | ||||||||
400012 | 11.0 | ||||||||
400013 | 8.0 | ||||||||
400014 | 26.0 | ||||||||
400015 | 38.0 | ||||||||
400016 | 0.5 | ||||||||
400017 | 0.5 | ||||||||
400018 | 6.0 |
------------------ |
Sample No. | Cs* | La* | Ce* | B* | Li* | Be* | Na* | Mg* | Al* |
JS-G1902 | 0.33 | 2.50 | 5.94 | 2 | 0 | 0 | 0 | 0 | |
JS-G1903 | 0.54 | 2.50 | 5.67 | 3 | 0 | 0 | 0 | 1 | |
JS-G1904 | 4.05 | 9.10 | 26.60 | 24 | 1 | 0 | 1 | 3 | |
JS-G1905 | -0.05 | -0.50 | 0.58 | 0 | -0 | 0 | 0 | 0 | |
JS-G1906 | 0.06 | -0.50 | 0.79 | 1 | -0 | 0 | 0 | 0 | |
JS-G1907 | 0.19 | 1.40 | 3.06 | 2 | -0 | 0 | 0 | 0 | |
JS-G1908 | -0.05 | -0.50 | 0.62 | 1 | -0 | 0 | 0 | 0 | |
JS-G1909 | 0.05 | -0.50 | 0.54 | 1 | -0 | 0 | 0 | 0 | |
ST0237.TGST93.058 | 1.00 | -3 | |||||||
ST0237.TGST93.059 | -1.00 | 10 | |||||||
ST0237.TGST93.060 | 3.00 | -3 | |||||||
ST0237.TGST93.061 | -1.00 | -3 | |||||||
ST0237.01 | -1.00 | -3 | |||||||
ST0237.02 | -1.00 | -3 | |||||||
ST0237.03 | -1.00 | -3 | |||||||
ST0237.04 | -1.00 | -3 | |||||||
ST0237.05 | 1.00 | -3 | |||||||
ST0237.06 | -1.00 | -3 | |||||||
ST0237.07 | -1.00 | -3 | |||||||
400011 | 0.50 | ||||||||
400012 | 0.50 | ||||||||
400013 | 1.00 | ||||||||
400014 | 1.00 | ||||||||
400015 | 4.00 | ||||||||
400016 | 0.50 | ||||||||
400017 | 0.50 | ||||||||
400018 | 0.50 |
------------------ |
Sample No. | P* | K * | Ca* | Sc* | Ti* | Te* | Hf* | Re* | Tl* |
JS-G1902 | 200 | 0 | 3 | 0.80 | 0 | 7.70 | 0.30 | 13 | 1 |
JS-G1903 | 230 | 0 | 1 | 0.80 | 0 | 2.46 | 0.40 | 5 | 2 |
JS-G1904 | 130 | 1 | 1 | 4.10 | 0 | 37.20 | 2.50 | 7 | 35 |
JS-G1905 | 50 | 0 | 0 | 0.10 | -0 | 11.25 | -0.10 | 12 | 1 |
JS-G1906 | 40 | 0 | 0 | 0.20 | -0 | 10.35 | -0.10 | 7 | 0 |
JS-G1907 | 180 | 0 | 0 | 0.40 | 0 | 5.68 | 0.10 | 3 | 2 |
JS-G1908 | 10 | 0 | 0 | 0.30 | -0 | 0.45 | 0.10 | 9 | 1 |
JS-G1909 | 20 | 0 | 0 | 0.10 | -0 | 8.53 | 0.10 | 5 | 0 |
ST0237.TGST93.058 | |||||||||
ST0237.TGST93.059 | |||||||||
ST0237.TGST93.060 | |||||||||
ST0237.TGST93.061 | |||||||||
ST0237.01 | |||||||||
ST0237.02 | |||||||||
ST0237.03 | |||||||||
ST0237.04 | |||||||||
ST0237.05 | |||||||||
ST0237.06 | |||||||||
ST0237.07 | |||||||||
400011 | 30 | ||||||||
400012 | 30 | ||||||||
400013 | 30 | ||||||||
400014 | 30 | ||||||||
400015 | 120 | ||||||||
400016 | 30 | ||||||||
400017 | 30 | ||||||||
400018 | 30 |
The fact sheet was created on 29.04.2024 |
Questions or comments regarding the fact sheet can be emailed to: ressursdatabaser@ngu.no |
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