Norsk versjon | |||||
THE ORE DATABASE | |||||
Deposit 4225 - 002 Flottorp | |||||
(Object Id: 5029) (Last updated: 15.03.2024) |
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Location |
County: | Agder | Municipality: | Lyngdal (4225) |
Map 1:50000: | Bjelland (1411-1) | Map 1:250000: | Mandal |
Coordinate system: | EU89-UTM Zone 32 |
East: | 404979 m. | North: | 6483260 m. |
Longitude: | 7.3705240 | Latitude: | 58.4796050 |
Show on map |
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Resource |
Resource Type: | Ferroalloys (Cr,Ni,Co,V,Mo,W) | Resource Subtype: | Molybdenium | |
Element(s): | Mo |
Importance |
Raw material meaning: | Not Assessed (reg. 18.02.2015) |
Resources and production |
Activity: | Mining | Reserves: | ||
Operating method: | Open pit and underground mining | Historical production: | 44,4 thousand tons |
Products |
Element/product | Crude ore grade or quality | Reg. date | |
Mo | 0,2 % | 13.03.2024 | |
MoS2 | 0.225 % | 07.01.2022 |
Operations |
From - To | Activity | Comments | |
1916 - 1919 | Regular production | Company/Institution :A/S Undalen Molybdengruber | |
1941 - 1942 | Detail mapping | Company/Institution :Raffineringsverket A/S |
Mineralization |
Era: | Proterozoic | Period: | Neoproterozoic | |
Dating: | 980 million year | Method: | ||
Genesis: | Form: | Irregular | ||
Main texture: | Structureless | Min. distribution: | Disseminated (<20 % ore minerals) |
Main grain size: | Very unevenly grained | Main alteration: |
Strike/Dip: | Direction: | |||
Plunge: |
Stratigraphic classification of host rock |
Era: | Proterozoic | Period: | Mesoproterozoic |
Province: | South Norwegian Basement Province | |
Geotec.unit: | Agder Complex | |
Tectonic complex: | Sirdal Magmatic Belt | |
Igneous complex: |
Group: | Formation: |
Mineralogy |
Relationship | Mineral | Amount | |
Gangue mineral | Feldspar | Major mineral (>10%) | |
Gangue mineral | Biotite | Major mineral (>10%) | |
Gangue mineral | Quartz | Major mineral (>10%) | |
Ore mineral | Molybdenite | Major mineral (>10%) | |
Ore mineral | Pyrite | Subordinate mineral (1-10%) | |
Ore mineral | Chalcopyrite | Subordinate mineral (1-10%) |
Lithology: |
Relationship | Rock | Origin | |
Host rock | Biotite gneiss | ||
Metamorphic facies :Amphibolite | |||
Wall rock | Granite | Intrusive Original rock :Granite |
Information(s) in free text format |
Free text |
In the period 1916–1919, around 48 000 t of ore with varying grades, 0.13 to 0.23 % MoS2, was produced from the two mines: Øvre and Ytre Flottorp (Undal) (olmsen 1961). Total recorded production of concentrate of molybdenite is 78 t (30-75 % MoS2, corresponding to 33 t of 100% MoS2, Bugge 1j963). The molybdenite occurrences are associated bands of 'amphibolitic', biotite-rich gneiss within granite/granitic gneiss. Mo-mineralisations occur in thin, molybdenite-bearing quartz and pegmatitic veins within the mafic gneiss and disseminations and joints of molybdenite enveloping the veins (Bugge 1963). |
Bibliography: |
From NGU's Reference Archive: |
Bugge, Arne , 1963 |
Norges molybdenforekomster. |
;Norges geologiske undersøkelse;TIDSSKRIFTARTIKKEL;NGU; No.217;1-134 pages |
Abstract: | |
The ore fields and individual deposits which are mentioned in the text are shown on the map, figure 2. For those areas where the deposits lie so close together that they cannot be shown separately on this map, detail maps have been drawn on larger scales. In the descriptions there will also be found special maps covering the most important molybdenum areas. An index of the deposits which are mentioned is arranged both alphabetically and according to the numbers on the map. The majority, including the most important, of the ore deposits in Southern Norway lie within a marked zone, which is shown on the map, figure 3. At varying periods of time different metals have characterised the long zone of ore deposits: titanium in the southwest, then molybdenum in the area from Gursli to Knaben, copper and molybdenum in Telemark, silver, zinc and lead from Kongsberg eastwards, and further to the east, molybdenum again. From the map, figure 4, it can be seen that the most important groups of deposits are situated to both sides of the granite-gneiss area of the mountanious region of Southern Norway and that they lie in migmatised gneisses along the southwest side and in the schists and quartzites of the Telemark supracrustal suite along the northeast side. |
Carstens, C. W.; Bjørlykke, H. , 1942 |
Flottorp molybdenskjerp. |
;Norges geologiske undersøkelse;FAGRAPPORT;Bergarkivet; No.BA 1409;12 pages |
Abstract: | |
Rapporten inneholder: 1. Kort malmgeologisk beskrivelse av Flottorp molybdenforekomst (4 s). 2. Malmgeologisk beskrivelse på bakgrunn av utførte diamantboringer (3 s). 3. Rapport over geologiske undersøkelser i 1942 av Flottorp Molybden- skjerp (3 s). 4. Sammendrag av utførte undersøkelser ved Flottorp molybdenforekomst (2s). |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||
JS-W2130 | Dump |
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JS-W2131 | Dump |
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JS-W2132 | Dump |
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NB! All analyse values are shown at the end of the printout.: |
Name of Locality: Undalen |
(Object Id: 38444 2,01,00) |
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Location |
County: | Agder | Municipality: | Lyngdal (4225) |
Map 1:50000: | Bjelland (1411-1) | Map 1:250000: | Mandal |
County: | (Unavailable) |
|
Resource |
Resource Type: | Ferroalloys (Cr,Ni,Co,V,Mo,W) | Resource Subtype: | Molybdenium | |
Element(s): | Mo |
Resources and production |
Activity: | Mining | Reserves: | ||
Operating method: | Open pit mining | Historical production: |
Analyse Results |
from |
Deposit Area 4225 - 002 Flottorp |
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-W2130 | Dump | 883 | 43 | 22 | 6 | 4 | .5 | -1.0 |
JS-W2131 | Dump | 997 | 52 | 25 | 6 | 6 | .5 | -1.0 |
JS-W2132 | Dump | 1960 | 81 | 32 | 12 | 6 | .9 | 4.0 |
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Sample No. | Pt# | Pd# | As* | Cd* | Ba* | Mo* | Sn* | Sb* | Bi* |
JS-W2130 | -5.0 | -1.0 | 1 | .2 | 730 | 7370.00 | 1 | -0 | 0 |
JS-W2131 | 8.0 | 1.0 | 0 | .2 | 890 | 8700.00 | 2 | 0 | 0 |
JS-W2132 | -5.0 | -1.0 | 0 | .6 | 960 | 9190.00 | 2 | 0 | 0 |
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Sample No. | Se* | Ga* | Ge* | In* | S% | V* | Cr* | Mn* | Fe% |
JS-W2130 | 3.00 | 17.95 | 0.09 | 0.05 | 1.00 | 29 | 8 | 229 | 2.47 |
JS-W2131 | 5.00 | 17.85 | 0.17 | 0.12 | 1.32 | 27 | 12 | 394 | 2.89 |
JS-W2132 | 5.00 | 23.00 | 0.18 | 0.12 | 1.82 | 34 | 11 | 367 | 4.06 |
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Sample No. | Th* | U* | W* | Rb* | Sr* | Y* | Zr* | Nb* | Ta* |
JS-W2130 | 2.83 | 1.40 | 1 | 146.5 | 216.0 | 10.1 | 202 | 3.00 | 0.06 |
JS-W2131 | 14.35 | 1.00 | 1 | 179.5 | 154.5 | 21.1 | 171 | 16.00 | 0.46 |
JS-W2132 | 16.10 | 1.00 | 1 | 251.0 | 233.0 | 25.3 | 185 | 13.30 | 0.39 |
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Sample No. | Cs* | La* | Ce* | Li* | Be* | Na* | Mg* | Al* | P* |
JS-W2130 | 0.70 | 22.00 | 42.50 | 5 | 2 | 21800 | 1900 | 63800 | 330 |
JS-W2131 | 1.06 | 54.60 | 117.00 | 8 | 2 | 17100 | 2700 | 58200 | 600 |
JS-W2132 | 1.58 | 72.60 | 160.00 | 10 | 2 | 22600 | 3600 | 75400 | 650 |
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Sample No. | K * | Ca* | Sc* | Ti* | Te* | Hf* | Re* | Tl* | |
JS-W2130 | 33800 | 9900 | 1.90 | 1930 | 0.20 | 5.80 | 0 | 1 | |
JS-W2131 | 36900 | 9100 | 4.50 | 2860 | 0.33 | 5.00 | 1 | 2 | |
JS-W2132 | 47800 | 10500 | 4.40 | 3590 | 0.57 | 5.30 | 0 | 2 |
The fact sheet was created on 04.05.2024 |
Questions or comments regarding the fact sheet can be emailed to: ressursdatabaser@ngu.no |
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