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THE ORE DATABASE | |||||
Deposit Area 1114 - 009 | |||||
(Last updated 10.jun.2015) |
Name of Deposit Area : Bjerkreim SW |
(Object Id : 1114,009,00,00) |
Location |
County : | Rogaland (11) | Municipality : | Bjerkreim (1114) |
Map 1:50000: | Bjerkreim (1212-2) | Map 1:250000: | Stavanger |
Marking point: | Longitude: | 6.0859530 | Latitude: | 58.5800230 |
EU89-UTM Zone 32 |
X-coord: | 330580 m. | Y-coord: | 6496966 m. |
|
Commodity |
Main Type: | Ferrous metals(Fe, Mn, Ti) | Sub Type: | Iron-Titanium | |
Element(s): | Fe Ti P V |
Production |
Activity: | Exploration | Reserves: | ||
Prod. method: | Production: | |||
Prod. status: | Volume of dump: |
Importance |
Public: | Not Assessed (reg. 10.06.2015) |
Economical: | Significant , (Confirmed 24.feb.2005 by Gurli Meyer) |
Operations |
From - To | Activity | Comments | |
1999 - 2005 | Geochemistry | Company/Institution :Geological Survey of Norway | |
The project has partly been financed by Norwegian Hydro (now Yara). | |||
2000 - 2004 | Detail mapping | Company/Institution :NGU/Henrik Schiellerup | |
Hand specimen sampling |
Mineralization |
Era: | Proterozoic | Period: | Mesoproterozoic | |
Dating: | 931 (-3\+3) million year | Method: | U/Pb | |
Genesis: | Orthomagmatic formation | Form: | Layer | |
Main texture: | Banded | Min. distribution: | Disseminated (<20 % ore minerals) |
Main grain size: | Medium grained (1-3 mm) | Main alteration: |
Strike/Dip: | 4 / 50 | Direction: | ||
Plunge: |
Ti-deposit type(s) |
Main type: | Magmatic | Ilm/Mt-ratio: | ||
Sub type: | Ilm +/- Mt +/- Ap in mafic intrusion | %TiO(Ore): | ||
Titanium province: | Rogaland anorthosite province | %P2O5(Ore): | ||
Host rock: | Norite | %MgO(Ilm): | 1 - 3 | |
Main Ti mineral: | Ilmenite | %V2O3(Mt): | > 0.8 | |
ppm U (Rutile): |
Stratigraphic classification of host rock |
Era: | Proterozoic | Period: | Mesoproterozoic |
Province: | South Norwegian Basement Province | |
Geotec.unit: | ||
Tectonic complex: | ||
Igneous complex: | Egersund Anorthosite Complex |
Group: | Bjerkreim-Sokndal Intrusion | Formation: |
Mineralogy |
Relationship | Mineral | Amount | |
Gangue mineral | Plagioclase | Major mineral (>10%) | |
Gangue mineral | Pyroxene | Major mineral (>10%) | |
Gangue mineral | Biotite | Accessory mineral (<1%) | |
Ore mineral | Ilmenite | Major mineral (>10%) | |
Ore mineral | Magnetite | Major mineral (>10%) | |
Ore mineral | Apatite | Subordinate mineral (1-10%) |
Lithology: |
Relationship | Rock | Origin | |
Host rock | Gabbronorite | Intrusive | |
Metamorphic facies :Unmetamorphosed |
Structures |
Location: | Type: | Orientation(360 gr.): | Relation to min.: | |
Host rock | Primary layering | Strike/Dip :4 / 50 | Syn-mineralisation ;...Effect :Controls |
Information(s) in free text format |
Abstract |
Oxide- and apatite-rich modally layered rocks in the lower part of the Bjerkreim-Sokndal Layered Intrusion in the Rogaland Anorthosite Province. The area is conventionally denoted MCUIB-e and defines a sequence of apatite-, ilmenite- and magnetite-bearing gabbronorite which may be followed from the farm at Åsen to Bjerkreim. The area is densely covered and the sequence only rarely exposed. The poor exposure makes it difficult to confidently assess the persistency and aerial extent of the MCU1Be target area. However, the overall similarities observed in profiles across the zone in terms of layering and mafic index do suggest that a prominent apatite-, ilmenite- and magnetite-rich zone exists. The zone varies in thickness from 15-20 to 60 m and is likely to be laterally continuous for at least 3 km wedging out gradually to the north and south. |
Description |
Megacyclic Unit (MCU) 1B distinguishes itself from the MCU's 3 and 4 in an important way: It does not contain any magnetite-bearing b- or d-zones, which means that the first appearance of apatite and magnetite is simultaneously at the base of zone MCU1Be. The MCU1Be is a relatively narrow zone of apatite, magnetite and ilmenite-rich cumulates extending south and southwest from the hinge zone of the intrusion near the village of Bjerkreim. The zone is 40-90 m wide and may be followed along strike for approximately 4 km. The stratigraphy has been offset by a number of minor faults. At the locality Bjerkreim SW, north of Berse lake, the zone is densely overgrown. It is therefore difficult to obtain a continuous impression of the extent and potential of the zone. The profile contains prominent sequences dominated by melanocratic apatite-, ilmenite- and magnetite-rich gabbronorite in intensely layered cumulates. 5 samples are taken in a profile and 1 sample at an isolated exposures south of Bjerkreim. The sequence here is not as extensive as at Åsen (< 50 m) and both the zone and the layered sequence tend to wedge out on approaching Bjerkreim. In the northernmost exposures, closer to Bjerkreim, the melanocratic series is only about 10 m thick and somewhat more leucocratic. The zone of economic interest is defined by 4 samples representing a 50 meter stratigraphis sequence of cumulates. Norm calculations from XRF whole rock analyses gives a total of 14.5% ilmenite, 10% magnetite and 7% apatite. The mineral composition of ilmenite and magnetite has been analysed by electron microprobe giving in average 1.5% MgO in ilmenite and 0.90% V2O3 in magnetite. |
Free text |
The deposit located at Bjerkreim SW corresponds to profile 2 and location 2 in the samplelist. It is part of the same zone (MCU1B-e) as the deposit descibed as Åsen (profile 1/ location 1). At the locality Bjerkreim SW, north of Berse lake, the zone is densely overgrown. It is therefore difficult to obtain a continuous impression of the extent and potential of the zone. The profile contains prominent sequences dominated by melanocratic apatite-, ilmenite- and magnetite-rich gabbronorite in intensely layered cumulates. 5 samples are taken in a profile and 1 sample at an isolated exposures south of Bjerkreim. The sequence here is not as extensive as at Åsen (< 50 m) and both the zone and the layered sequence tend to wedge out on approaching Bjerkreim. In the northernmost exposures, closer to Bjerkreim, the melanocratic series is only about 10 m thick and somewhat more leucocratic. The zone of economic interest is defined by 4 samples representing a 50 meter stratigraphis sequence of cumulates. Norm calculations from XRF whole rock analyses gives a total of 14.5% ilmenite, 10% magnetite and 7% apatite. The mineral composition of ilmenite and magnetite has been analysed by electron microprobe giving in average 1.5% MgO in ilmenite and 0.90% V2O3 in magnetite. |
References |
Schärer, U., E. Wilmart, et al. (1996). ¿The short duration and anorogenic character of anorthosite magmatism: U-Pb dating of the Rogaland complex, Norway.¿ Earth Planet. Sci. Lett. 139: 335-350. Egersund-Ogna: 929±2 Ma Helleren: 932±3 Ma Åna-Sira: 932±3 Ma Tellnes jotunite dyke: 931±5 Ma Tellnes ilmenite norite: 920±3 Ma Deformation of foliated margin in Egersund-Ogna: 915 Ma |
Photo(s) from the Deposit area: |
|
Bibliography: |
From NGU's Reference Archive: |
Korneliussen, Are; McEnroe, Suzanne A.; Nilsson, Lars-Petter; Schiellerup, Henrik; Gautneb, Håvard; Meyer, Gurli B.; Størseth, Leif Roger , 2000 |
An overview of titanium deposits in Norway |
;Norges geologiske undersøkelse;TIDSSKRIFTARTIKKEL;NGU Bulletin; No.436;27-38 pages |
Abstract: | |
Titanium deposits in Norway are of three major types: igneous, metasomatic and metamorphic. The igneous deposits are compared of ilmenite, magnetite and apatite in various proportions and occur in geological provinces of different ages. and some have a metamorphic overprint. The other majord Ti ore-types is the rutile-bearing eclogites in western Norway that formed during the Caledonian high-pressure metamorphism of predominantly Proterozoic basic igneous rocks. The third Ti ore-Type is the Proterozoic rutile-bearing, scapolitised and albitised rocks in the Bamble region of South Norway. |
Meyer, G.B.; Schiellerup, H.; Tegner, C. , 2002 |
Chemical characterisation of ilmenite, magnetite and apatite in the Bjerkreim-Sokndal Layered Intrusion, Rogaland, South Norway |
;Norges geologiske undersøkelse;FAGRAPPORT;NGU-rapport; No.2002.042;25 pages |
Abstract: | |
During 2001 cooperation was established between NGU and Norsk Hydro Agri in order to locate combined resources of apatite, ilmenite and vanadium magnetite in the Bjerkreim-Sokndal layered Intrusion in the Rogaland Anorthosite Province of aouth Norway. It had previously been recognized that a potential existed for finding coexisting apatite, low-Mg= ilmenite and vanadium-rich magnetite in the northern part (the Bjerkreim-lobe) of the layered intrusion. It had also become apparent that none of the minerals are present in amounts that can support exploitation of one mineral alone. Fieldwork was undertaken during July 2001 with the purpose of locating and constraining the most promising areas in terms of volume and grade of the three target minerals in the Bjerkreim-lobe. Three apatite-bearing and oxide-rich zones were singled out, sampled and preliminarily constrained. These zones are located with one area in mega-cyclic unit (MCU) IBe (Åsen-Bjerkreim), containing up to 41% of the three minerals, two areas in MCU IIIe (Helland and Terland respectively), with up to 34% of the three minerals, and in MCU IVe (Teksevatnet-Vasshus), with 32% ilmenite, magnetite and apatite. The fieldwork and subsequent whole-rock chemical analyses (XRF) were described and discussed by Schiellerup et al. (2001). In the apatite. and oxide-rich part of MCU IBe the MgO-content of ilmenite vary between 1.36 and 2.26% with an average of 1.8%. Stratigraphically dependant variation has not been resolved and the highest MgO contents in ilmenite tend to occur in the most mafic layers. In the two MCU III prospects at Helleland and Terland the MgO-content in ilmenite averages 2.2 and 2.5% respectively, whereas the Teksevatnet profile yield an average of 1.4% MgO in ilmenite. In the Teksevatnet profile the modal contrast between mafic and felsic layers is exceptional and the MgO-content of ilmenite is consi |
Schiellerup, H.; Meyer, G.B.; Tegner, C.; Robins, B.; Korneliussen, A. , 2001 |
Resources of apatite, ilmenite and magnetite in the Bjerkreim Sokndal Layered Intrusion, Rogaland, South Norway |
;Norges geologiske undersøkelse;FAGRAPPORT;NGU-rapport; No.2001.092;33 pages |
Abstract: | |
The Rogaland Anorthosite Province in southwest Norway is well known for its many ilmenite deposits, of which Tellnes is at present the only one in product- ion In addition to ilmenite, the province carries a significant potential for apatite and vanadium-rich magnetite occurring in the layered series of the Bjerkreim-Sokndal Layered Intrusion. The current study was undertaken in order to locate exploitable resources of combined apatite, ilmenite and vanadian magnetite in the Bjerkreim-lobe of the Bjerkreim-Sokndal intrusion. |
Korneliussen, A.; Furuhaug, L.; Gautneb, H.; McEnroe, S.; Nilsson, L.P.; Sørdal, T. , 2001 |
Forekomster med ilmenitt, vanadiumholdig magnetitt og apatitt i norittiske bergarter i Egersundfeltet, Rogaland |
;Norges geologiske undersøkelse;FAGRAPPORT;NGU-rapport; No.2001.014;29 pages |
Abstract: | |
Ved tidligere undersøkelser er det påvist at norittiske bergarter i omrpåden Sokndal og Bjerkreim inneholder betydelige mengder av apatitt, ilmenitt og vanadiumholdig magnetitt, men at forekomstene er lavgehaltige. En rekke norittrelaterte forekomster inneholder i størrelsesorden 10% apatitt, 10% ilmenitt og 10% magnetitt. De minerallogiske kvaliteter synes å være gode. For eksempel forekommer ilmenitt med relativt lavt MgO-innhold (i størrelsesorden 1%) og magnetitt med høyt V-innhold (0.7-1.2% V2O2) sammen med C1-fattig apatitt i visse deler av området, noe som er positivt med tanke på mulighetene for framtidig gruvedrift. Samtidig er de samlede ressurser av kombinert apatitt ilmenitt og vanadiumrik magnetitt store. Og det burde være rimelig gode muligheter til å påvise nye forekomster med minst like gode kvaliteter som de som er påvist fram til nå. |
Name of Sample point : NH-72 |
(Object Id : 1114,009,02,01) |
Location |
County : | Rogaland (11) | Municipality : | Bjerkreim (1114) |
Map 1:50000: | Bjerkreim (1212-2) | Map 1:250000: | Stavanger |
Marking point: | Longitude: | 6.0851390 | Latitude: | 58.5799890 |
EU89-UTM Zone 32 |
X-coord: | 330532 m. | Y-coord: | 6496964 m. |
|
Commodity |
Main Type: | Ferrous metals(Fe, Mn, Ti) | Sub Type: | Iron-Titanium | |
Element(s): | Fe Ti P V |
Information(s) in free text format |
Description |
MCU 1B-e. Magnetite-apatite gabbronorite. Less melanocratic than NH-71. 20 cm below NH-71. Relative stratigraphis height in profile 2: 0 m |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | |||||
NH-72 | Bedrock |
|
NB! All analyse values are shown at the end of the printout.: |
Name of Sample point : NH-71 |
(Object Id : 1114,009,02,02) |
Location |
County : | Rogaland (11) | Municipality : | Bjerkreim (1114) |
Map 1:50000: | Bjerkreim (1212-2) | Map 1:250000: | Stavanger |
Marking point: | Longitude: | 6.0851390 | Latitude: | 58.5799890 |
EU89-UTM Zone 32 |
X-coord: | 330532 m. | Y-coord: | 6496964 m. |
|
Commodity |
Main Type: | Ferrous metals(Fe, Mn, Ti) | Sub Type: | Iron-Titanium | |
Element(s): | Fe Ti P V |
Information(s) in free text format |
Description |
MCU 1B-e. Magnetite-apatite gabbronorite from dark layer in 15-20 m thick layered sequence. In forest to the N of small farm some tens of metres above new road cut. Relative stratigraphic height in profile 2: 0 m |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | |||||
NH-71 | Bedrock |
|
NB! All analyse values are shown at the end of the printout.: |
Name of Sample point : NH-70 |
(Object Id : 1114,009,02,03) |
Location |
County : | Rogaland (11) | Municipality : | Bjerkreim (1114) |
Map 1:50000: | Bjerkreim (1212-2) | Map 1:250000: | Stavanger |
Marking point: | Longitude: | 6.0863280 | Latitude: | 58.5801780 |
EU89-UTM Zone 32 |
X-coord: | 330603 m. | Y-coord: | 6496982 m. |
|
Commodity |
Main Type: | Ferrous metals(Fe, Mn, Ti) | Sub Type: | Iron-Titanium | |
Element(s): | Fe Ti P V |
Information(s) in free text format |
Description |
Melanocratic magnetite-apatite norite with abundant visible apatite. Sample locality few dm¿s from NH-69. Relative stratigraphic height in profile 2: 42 m |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | |||||
NH-70 | Bedrock |
|
NB! All analyse values are shown at the end of the printout.: |
Name of Sample point : NH-69 |
(Object Id : 1114,009,02,04) |
Location |
County : | Rogaland (11) | Municipality : | Bjerkreim (1114) |
Map 1:50000: | Bjerkreim (1212-2) | Map 1:250000: | Stavanger |
Marking point: | Longitude: | 6.0863280 | Latitude: | 58.5801780 |
EU89-UTM Zone 32 |
X-coord: | 330603 m. | Y-coord: | 6496982 m. |
|
Commodity |
Main Type: | Ferrous metals(Fe, Mn, Ti) | Sub Type: | Iron-Titanium | |
Element(s): | Fe Ti P V |
Information(s) in free text format |
Description |
Relatively leucocratic layer c. 10 m stratigraphically below NH-68. Sample not particular leucocratic though. Relative stratigraphic height in profile 2: 42 m |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | |||||
NH-69 | Bedrock |
|
NB! All analyse values are shown at the end of the printout.: |
Name of Sample point : NH-68 |
(Object Id : 1114,009,02,05) |
Location |
County : | Rogaland (11) | Municipality : | Bjerkreim (1114) |
Map 1:50000: | Bjerkreim (1212-2) | Map 1:250000: | Stavanger |
Marking point: | Longitude: | 6.0864760 | Latitude: | 58.5798490 |
EU89-UTM Zone 32 |
X-coord: | 330610 m. | Y-coord: | 6496945 m. |
|
Commodity |
Main Type: | Ferrous metals(Fe, Mn, Ti) | Sub Type: | Iron-Titanium | |
Element(s): | Fe Ti P V |
Information(s) in free text format |
Description |
Top of melanocratic sequence below base MCU II. The top c. 10+ m of MCU IA do not display pronounced modal layering, but are overall fairly melanocratic. The layered melanocratic sequence below this zone has a thickness on the order of 20m. NH-68 from top of layered melanocratic sequence phaimC. Relative stratigraphic height in profile 2: 51 m |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | |||||
NH-68 | Bedrock |
|
NB! All analyse values are shown at the end of the printout.: |
Name of Sample point : NH-74 |
(Object Id : 1114,009,02,06) |
Location |
County : | Rogaland (11) | Municipality : | Bjerkreim (1114) |
Map 1:50000: | Bjerkreim (1212-2) | Map 1:250000: | Stavanger |
Marking point: | Longitude: | 6.0890940 | Latitude: | 58.5827130 |
EU89-UTM Zone 32 |
X-coord: | 330775 m. | Y-coord: | 6497258 m. |
|
Commodity |
Main Type: | Ferrous metals(Fe, Mn, Ti) | Sub Type: | Iron-Titanium | |
Element(s): | Fe Ti P V |
Information(s) in free text format |
Description |
MCU 1B-e. Not in actual sequence with NH-68-72, but somewhat further to the northeast along strike. Magnetite-apatite gabbronorite from diffuse melanocratic layer in the middle portion of section (almost average rock). Layering in this sequence strikes N020 and dips 40° to the E. This section is more than 10 m thick and sampled at farm road. It is dominated by normal magnetite gabbronorite with apatite. Intermittent dark layers 5-15 cm thick. Many melanocratic magnetite-apatite gabbronorite loose blocks in the area. |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | |||||
NH-74 | Bedrock |
|
NB! All analyse values are shown at the end of the printout.: |
Analyse Results |
from |
Deposit Area 1114 - 009 Bjerkreim SW |
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* | As* |
NH-68 | Bedrock | 93 | 133 | 5 | 83 | 25 | 5.0 | 5 |
NH-69 | Bedrock | 45 | 130 | 5 | 61 | 14 | 5.0 | 5 |
NH-70 | Bedrock | 43 | 154 | 5 | 84 | 20 | 5.0 | 5 |
NH-71 | Bedrock | 45 | 112 | 5 | 67 | 22 | 5.0 | 5 |
NH-72 | Bedrock | 42 | 57 | 5 | 50 | 22 | 5.0 | 5 |
NH-74 | Bedrock | 35 | 54 | 5 | 42 | 20 | 5.0 | 5 |
------------------ |
Sample No. | Cd* | Ba* | Mo* | Sn* | Sb* | Ga* | S% | V* | Cr* |
NH-68 | 5.0 | 51 | 2.50 | 5 | 5 | 23.00 | .05 | 525 | 5 |
NH-69 | 5.0 | 50 | 2.50 | 5 | 5 | 22.00 | .05 | 525 | 5 |
NH-70 | 5.0 | 31 | 2.50 | 5 | 5 | 19.00 | .05 | 508 | 5 |
NH-71 | 5.0 | 93 | 2.50 | 5 | 5 | 28.00 | .05 | 522 | 5 |
NH-72 | 5.0 | 190 | 2.50 | 5 | 5 | 30.00 | .05 | 335 | 5 |
NH-74 | 5.0 | 190 | 2.50 | 5 | 5 | 27.00 | .05 | 376 | 5 |
------------------ |
Sample No. | Fe% | Th* | U* | W* | Rb* | Sr* | Y* | Zr* | Nb* |
NH-68 | ###### | 5.00 | 5.00 | 15 | 2.5 | 143.0 | 17.0 | 15 | 2.50 |
NH-69 | ###### | 5.00 | 5.00 | 15 | 2.5 | 170.0 | 22.0 | 13 | 2.50 |
NH-70 | ###### | 5.00 | 5.00 | 15 | 2.5 | 99.0 | 18.0 | 17 | 2.50 |
NH-71 | ###### | 5.00 | 5.00 | 15 | 2.5 | 273.0 | 23.0 | 13 | 2.50 |
NH-72 | ###### | 5.00 | 5.00 | 15 | 2.5 | 490.0 | 23.0 | 9 | 2.50 |
NH-74 | ###### | 5.00 | 13.00 | 15 | 2.5 | 439.0 | 17.0 | 10 | 2.50 |
------------------ |
Sample No. | La* | Ce* | Nd* | Yb* | F* | P* | Cl* | Sc* | Ti* |
NH-68 | 14.00 | 7.50 | 49.00 | 8.00 | 0 | 60956 | 0 | 40.00 | ###### |
NH-69 | 11.00 | 7.50 | 56.00 | 8.00 | 0 | 69893 | 0 | 42.00 | ###### |
NH-70 | 24.00 | 7.50 | 59.00 | 8.00 | 0 | 59352 | 0 | 53.00 | ###### |
NH-71 | 24.00 | 7.50 | 55.00 | 8.00 | 0 | 71268 | 0 | 43.00 | ###### |
NH-72 | 5.00 | 29.00 | 35.00 | 8.00 | 0 | 67601 | 0 | 25.00 | 65746 |
NH-74 | 5.00 | 24.00 | 26.00 | 8.00 | 0 | 64164 | 0 | 24.00 | 63577 |
Oxide analyses |
( All values are in % ) |
Sample No. | Sample Type | SiO2 | Al2O3 | TiO2 | Fe2O3 | MnO | MgO | CaO |
NH-68 | Bedrock | 35.49 | 5.26 | 7.28 | 27.32 | 0.19 | 11.20 | 9.94 |
NH-69 | Bedrock | 35.99 | 5.64 | 7.33 | 25.68 | 0.20 | 10.75 | 10.21 |
NH-70 | Bedrock | 34.35 | 3.75 | 8.34 | 28.63 | 0.23 | 12.09 | 9.11 |
NH-71 | Bedrock | 37.03 | 8.67 | 6.52 | 23.20 | 0.17 | 8.69 | 9.83 |
NH-72 | Bedrock | 44.15 | 15.16 | 3.94 | 14.09 | 0.10 | 5.15 | 10.68 |
NH-74 | Bedrock | 44.64 | 15.94 | 3.81 | 13.13 | 0.09 | 4.70 | 10.71 |
------------------ |
Sample No. | Na2O | K2O | P2O5 | Sum | |||||
NH-68 | 0.75 | 0.11 | 2.66 | 100.00 | |||||
NH-69 | 0.94 | 0.11 | 3.05 | 100.00 | |||||
NH-70 | 0.50 | 0.06 | 2.59 | 100.00 | |||||
NH-71 | 1.64 | 0.25 | 3.11 | 99.00 | |||||
NH-72 | 3.30 | 0.47 | 2.95 | 100.00 | |||||
NH-74 | 3.49 | 0.51 | 2.80 | 100.00 |
The fact sheet was created on 20.01.2025 |
Questions or comments regarding the fact sheet can be emailed to: ressursdatabaser@ngu.no |
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