Östanmossa mine, Röberg ore field, Norberg, Västmanland County, Swedeni
| Regional Level Types | |
|---|---|
| Östanmossa mine | Mine (Abandoned) |
| Röberg ore field | Ore Field |
| Norberg | Municipality |
| Västmanland County | County |
| Sweden | Country |
Östanmossa mine, Röberg ore field, Bergslagen mining district, Sweden
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Latitude & Longitude (WGS84):
60° 4' 59'' North , 15° 55' 59'' East
Latitude & Longitude (decimal):
Type:
Mine (Abandoned) - last checked 2024
Köppen climate type:
Name(s) in local language(s):
Östanmossagruvan (Östanmossgruvan), Röbergsfältet , Norberg, Västmanland, Sverige
The Östanmossa deposit is the type locality for dollaseite-(Ce), arrheniusite-(Ce), and norbergite.
The Östanmossa mine produced iron ore from a skarn in the period from 1859 to 1934. The mine is worked to a depth of 114.9m. The Östanmossa mine is a Bastnäs-type REE deposit, belonging to the subtype (2) of Sahlström (Norberg type) in that it is enriched in heavy REE (HREE), Y, Mg, Ca, and F. The REE deposits are hosted in skarns associated with marble horizons in a strongly Na, K, and/or Mg-altered, metavolcanic succession.
The Östanmossa mines consist of a narrow zone of skarn in association with sporadic carbonate remnants, occurring within a stratified metavolcanic sequence with minor intercalated banded quartz-rich iron horizons. Closer to the skarn orebody, the volcanic host rocks are to some extent altered into mica- and quartz-rich rocks. The carbonate is a fine-grained dolomitic or coarse-grained calcitic marble, often in the form of an ophicalcite with (altered) humite minerals. The most extensive REE-mineralisation was encountered in the drift Grodorten at the 47 m level, consisting of an up to 20 m long zone following a contact between magnetite-amphibole skarn and a tremolite-bearing dolomitic marble.
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsCommodity List
This is a list of exploitable or exploited mineral commodities recorded at this locality.Mineral List
26 valid minerals. 3 (TL) - type locality of valid minerals.
Rock Types Recorded
Note: data is currently VERY limited. Please bear with us while we work towards adding this information!
Select Rock List Type
Alphabetical List Tree DiagramDetailed Mineral List:
| ⓘ Actinolite Formula: ◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2 |
| ⓘ 'Allanite Group' Formula: (A12+REE3+)(M13+M23+M32+)O[Si2O7][SiO4](OH) Description: The composition of the various grains and crystals of allanite group minerals are of an intermediate composition between dissakisite-(Ce), dollaseite-(Ce) and allanite-(Ce). Jansson (2001) distinguishes between dissakisite-(Ce) and dollaseite-(Ce) based on paragenesis. Small, anhedral grains and masses embedded in tremolite and larger tabular crystals embedded in calcite lenses within the tremolite are considered to be dissakisite-(Ce), whereas the material embedded in the dolomite marble associated with norbergite and magnetite is considered to be dollaseite-(Ce). The analytical basis for this distinction is quite slim.
|
| ⓘ 'Amphibole Supergroup' Formula: AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
| ⓘ Åsgruvanite-(Ce) Formula: Ce16Ca5Al(SiO4)6(AsO3)8(CO3)2Cl4F3(OH)2 References: Taddei, A.; Holtstam, D.; Jonsson, E.; Förster, H.-J.; Andersson, S. S.; Appelt, O.; Bindi, L. (2025) Exploring the unusual occurrence, chemistry, and structural topology of \aasgruvanite-(Ce), Ce₁₆Ca₅Al(SiO₄)₆(AsO₃)₈(CO₃)₂Cl₃(ClF₃)(OH)₂, a new rare earth element (REE) mineral from Västmanland, Sweden. European Journal of Mineralogy, 37 (6). 937-951 doi:10.5194/ejm-37-937-2025 |
| ⓘ Arrheniusite-(Ce) (TL) Formula: CaMg[(Ce7Y3)Ca5](SiO4)4(Si2B3AsO18)(BO3)F11 Type Locality: References: Miyawaki, Ritsuro, Hatert, Frédéric, Pasero, Marco, Mills, Stuart J. (2020) IMA Commission on New Minerals, Nomenclature and Classification (CNMNC) – Newsletter 53. European Journal of Mineralogy, 32 (1) 209-213 doi:10.5194/ejm-32-209-2020 Holtstam, Dan; Bindi, Luca; Bonazzi, Paola; Förster, Hans-Jürgen; Andersson, Ulf B. (2021) Arrheniusite-(Ce), CaMg[(Ce7Y3)Ca5](SiO4)3(Si3B3O18)(AsO4)(BO3)F11, a New Member of the Vicanite Group, from the Östanmossa Mine, Norberg, Sweden. The Canadian Mineralogist, 59 (1). 177-189 doi:10.3749/canmin.2000045 |
| ⓘ Bastnäsite-(Ce) Formula: Ce(CO3)F Colour: Yellowgreen Description: See photo |
| ⓘ Bismuthinite Formula: Bi2S3 |
| ⓘ Calcite Formula: CaCO3 |
| ⓘ Cerite-(CeCa) ? Formula: (Ce7Ca2)◻Mg(SiO4)3(SiO3OH)4(OH)3 |
| ⓘ Chalcopyrite Formula: CuFeS2 |
| ⓘ 'Chlorite Group' |
| ⓘ Chondrodite Formula: Mg5(SiO4)2F2 Description: Chondrodite is found in an association with allanite-(Ce), tremolite and magnetite. |
| ⓘ Clinohumite Formula: Mg9(SiO4)4F2 Colour: orange Description: Clinohumite (and chondrodite?) is quite common in the ophicalcite where it occurs as small orange aggregates together with calcite and serpentine, sometimes also together with fluorite. |
| ⓘ Dissakisite-(Ce) Formula: (CaCe)(AlAlMg)O[Si2O7][SiO4](OH) Habit: massive Colour: red-brown, chocolate brown to black Description: Both subaluminous, ferroan dissakisite-(Ce) and Fe-poor dollaseite-(Ce) occurs at Östanmossa Mine (Grew et al. 1991). The composition of the various grains and crystals of allanite group minerals are of an intermediate composition between dissakisite-(Ce), dollaseite-(Ce) and allanite-(Ce). Jansson (2001) distinguishes between dissakisite-(Ce) and dollaseite-(Ce) based on paragenesis. Small, anhedral grains and masses embedded in tremolite and larger tabular crystals embedded in calcite lenses within the tremolite are considered to be dissakisite-(Ce), whereas the material embedded in the dolomite marble associated with norbergite and magnetite is considered to be dollaseite-(Ce). The analytical basis for this distinction is quite slim.
The individual grains embedded in tremolite are rarely visible to the naked eye, whereas the tabular crystals found embedded in calcite lenses in tremolite can be up to up to 4-10 mm. |
| ⓘ Dollaseite-(Ce) (TL) Formula: (CaCe)(MgAlMg)F[Si2O7][SiO4](OH) Type Locality: Habit: massive Colour: Brown Description: The composition of the various grains and crystals of allanite group minerals are of an intermediate composition between dissakisite-(Ce), dollaseite-(Ce) and allanite-(Ce). Jansson (2001) distinguishes between dissakisite-(Ce) and dollaseite-(Ce) based on paragenesis. Small, anhedral grains and masses embedded in tremolite and larger tabular crystals embedded in calcite lenses within the tremolite are considered to be dissakisite-(Ce), whereas the material embedded in the dolomite marble associated with norbergite and magnetite is considered to be dollaseite-(Ce). The analytical basis for this distinction is quite slim.
|
| ⓘ Dolomite Formula: CaMg(CO3)2 |
| ⓘ Fluorbritholite-(Ce) Formula: (Ce,Ca)5(SiO4)3F |
| ⓘ Fluorbritholite-(Y) Formula: (Y,Ca)5(SiO4)3F |
| ⓘ Gadolinite-(Ce) Formula: (Ce,La,Nd,Y)2Fe2+Be2Si2O10 Habit: microscopic granular Colour: green |
| ⓘ Gadolinite-(Y) Formula: Y2Fe2+Be2Si2O10 |
| ⓘ Humite Formula: Mg7(SiO4)3F2 |
| ⓘ Magnetite Formula: Fe2+Fe3+2O4 |
| ⓘ Molybdenite Formula: MoS2 |
| ⓘ Norbergite (TL) Formula: Mg3(SiO4)F2 Type Locality: Colour: pink, white, purplish Description: NOrbergite occurs as massive occurs in massive pink (purplish) to white aggregates and is associated with tremolite and an epidote group minerals. Only massive aggregates have been found Östanmossa iron mine |
| ⓘ Parisite-(Ce) Formula: CaCe2(CO3)3F2 |
| ⓘ Phlogopite Formula: KMg3(AlSi3O10)(OH)2 |
| ⓘ Pyrite Formula: FeS2 |
| ⓘ Quartz Formula: SiO2 |
| ⓘ Tremolite Formula: ◻Ca2Mg5(Si8O22)(OH)2 |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 2 - Sulphides and Sulfosalts | |||
|---|---|---|---|
| ⓘ | Chalcopyrite | 2.CB.10a | CuFeS2 |
| ⓘ | Bismuthinite | 2.DB.05 | Bi2S3 |
| ⓘ | Molybdenite | 2.EA.30 | MoS2 |
| ⓘ | Pyrite | 2.EB.05a | FeS2 |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | Magnetite | 4.BB.05 | Fe2+Fe3+2O4 |
| ⓘ | Quartz | 4.DA.05 | SiO2 |
| Group 5 - Nitrates and Carbonates | |||
| ⓘ | Calcite | 5.AB.05 | CaCO3 |
| ⓘ | Dolomite | 5.AB.10 | CaMg(CO3)2 |
| ⓘ | Bastnäsite-(Ce) | 5.BD.20a | Ce(CO3)F |
| ⓘ | Parisite-(Ce) | 5.BD.20b | CaCe2(CO3)3F2 |
| Group 9 - Silicates | |||
| ⓘ | Norbergite (TL) | 9.AF.40 | Mg3(SiO4)F2 |
| ⓘ | Chondrodite | 9.AF.45 | Mg5(SiO4)2F2 |
| ⓘ | Humite | 9.AF.50 | Mg7(SiO4)3F2 |
| ⓘ | Clinohumite | 9.AF.55 | Mg9(SiO4)4F2 |
| ⓘ | Cerite-(CeCa) ? | 9.AG.20 | (Ce7Ca2)◻Mg(SiO4)3(SiO3OH)4(OH)3 |
| ⓘ | Fluorbritholite-(Ce) | 9.AH.25 | (Ce,Ca)5(SiO4)3F |
| ⓘ | Fluorbritholite-(Y) | 9.AH.25 | (Y,Ca)5(SiO4)3F |
| ⓘ | Arrheniusite-(Ce) (TL) | 9.AJ. | CaMg[(Ce7Y3)Ca5](SiO4)4(Si2B3AsO18)(BO3)F11 |
| ⓘ | Gadolinite-(Ce) | 9.AJ.20 | (Ce,La,Nd,Y)2Fe2+Be2Si2O10 |
| ⓘ | Gadolinite-(Y) | 9.AJ.20 | Y2Fe2+Be2Si2O10 |
| ⓘ | Dollaseite-(Ce) (TL) | 9.BG.05 | (CaCe)(MgAlMg)F[Si2O7][SiO4](OH) |
| ⓘ | Dissakisite-(Ce) | 9.BG.05b | (CaCe)(AlAlMg)O[Si2O7][SiO4](OH) |
| ⓘ | Actinolite | 9.DE.10 | ◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2 |
| ⓘ | Tremolite | 9.DE.10 | ◻Ca2Mg5(Si8O22)(OH)2 |
| ⓘ | Phlogopite | 9.EC.20 | KMg3(AlSi3O10)(OH)2 |
| ⓘ | Åsgruvanite-(Ce) | 9.FB. | Ce16Ca5Al(SiO4)6(AsO3)8(CO3)2Cl4F3(OH)2 |
| Unclassified | |||
| ⓘ | 'Amphibole Supergroup' | - | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
| ⓘ | 'Chlorite Group' | - | |
| ⓘ | 'Allanite Group' | - | (A12+REE3+)(M13+M23+M32+)O[Si2O7][SiO4](OH) |
List of minerals for each chemical element
| H | Hydrogen | |
|---|---|---|
| H | ⓘ Actinolite | ◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2 |
| H | ⓘ Amphibole Supergroup | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
| H | ⓘ Cerite-(CeCa) | (Ce7Ca2)◻Mg(SiO4)3(SiO3OH)4(OH)3 |
| H | ⓘ Dissakisite-(Ce) | (CaCe)(AlAlMg)O[Si2O7][SiO4](OH) |
| H | ⓘ Dollaseite-(Ce) | (CaCe)(MgAlMg)F[Si2O7][SiO4](OH) |
| H | ⓘ Phlogopite | KMg3(AlSi3O10)(OH)2 |
| H | ⓘ Tremolite | ◻Ca2Mg5(Si8O22)(OH)2 |
| H | ⓘ Allanite Group | (A12+REE3+)(M13+M23+M32+)O[Si2O7][SiO4](OH) |
| H | ⓘ Åsgruvanite-(Ce) | Ce16Ca5Al(SiO4)6(AsO3)8(CO3)2Cl4F3(OH)2 |
| Be | Beryllium | |
| Be | ⓘ Gadolinite-(Ce) | (Ce,La,Nd,Y)2Fe2+Be2Si2O10 |
| Be | ⓘ Gadolinite-(Y) | Y2Fe2+Be2Si2O10 |
| B | Boron | |
| B | ⓘ Arrheniusite-(Ce) | CaMg[(Ce7Y3)Ca5](SiO4)4(Si2B3AsO18)(BO3)F11 |
| C | Carbon | |
| C | ⓘ Bastnäsite-(Ce) | Ce(CO3)F |
| C | ⓘ Calcite | CaCO3 |
| C | ⓘ Dolomite | CaMg(CO3)2 |
| C | ⓘ Parisite-(Ce) | CaCe2(CO3)3F2 |
| C | ⓘ Åsgruvanite-(Ce) | Ce16Ca5Al(SiO4)6(AsO3)8(CO3)2Cl4F3(OH)2 |
| O | Oxygen | |
| O | ⓘ Actinolite | ◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2 |
| O | ⓘ Amphibole Supergroup | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
| O | ⓘ Bastnäsite-(Ce) | Ce(CO3)F |
| O | ⓘ Calcite | CaCO3 |
| O | ⓘ Cerite-(CeCa) | (Ce7Ca2)◻Mg(SiO4)3(SiO3OH)4(OH)3 |
| O | ⓘ Chondrodite | Mg5(SiO4)2F2 |
| O | ⓘ Clinohumite | Mg9(SiO4)4F2 |
| O | ⓘ Dissakisite-(Ce) | (CaCe)(AlAlMg)O[Si2O7][SiO4](OH) |
| O | ⓘ Dollaseite-(Ce) | (CaCe)(MgAlMg)F[Si2O7][SiO4](OH) |
| O | ⓘ Dolomite | CaMg(CO3)2 |
| O | ⓘ Fluorbritholite-(Ce) | (Ce,Ca)5(SiO4)3F |
| O | ⓘ Gadolinite-(Ce) | (Ce,La,Nd,Y)2Fe2+Be2Si2O10 |
| O | ⓘ Gadolinite-(Y) | Y2Fe2+Be2Si2O10 |
| O | ⓘ Humite | Mg7(SiO4)3F2 |
| O | ⓘ Magnetite | Fe2+Fe23+O4 |
| O | ⓘ Norbergite | Mg3(SiO4)F2 |
| O | ⓘ Parisite-(Ce) | CaCe2(CO3)3F2 |
| O | ⓘ Phlogopite | KMg3(AlSi3O10)(OH)2 |
| O | ⓘ Quartz | SiO2 |
| O | ⓘ Tremolite | ◻Ca2Mg5(Si8O22)(OH)2 |
| O | ⓘ Fluorbritholite-(Y) | (Y,Ca)5(SiO4)3F |
| O | ⓘ Allanite Group | (A12+REE3+)(M13+M23+M32+)O[Si2O7][SiO4](OH) |
| O | ⓘ Arrheniusite-(Ce) | CaMg[(Ce7Y3)Ca5](SiO4)4(Si2B3AsO18)(BO3)F11 |
| O | ⓘ Åsgruvanite-(Ce) | Ce16Ca5Al(SiO4)6(AsO3)8(CO3)2Cl4F3(OH)2 |
| F | Fluorine | |
| F | ⓘ Amphibole Supergroup | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
| F | ⓘ Bastnäsite-(Ce) | Ce(CO3)F |
| F | ⓘ Chondrodite | Mg5(SiO4)2F2 |
| F | ⓘ Clinohumite | Mg9(SiO4)4F2 |
| F | ⓘ Dollaseite-(Ce) | (CaCe)(MgAlMg)F[Si2O7][SiO4](OH) |
| F | ⓘ Fluorbritholite-(Ce) | (Ce,Ca)5(SiO4)3F |
| F | ⓘ Humite | Mg7(SiO4)3F2 |
| F | ⓘ Norbergite | Mg3(SiO4)F2 |
| F | ⓘ Parisite-(Ce) | CaCe2(CO3)3F2 |
| F | ⓘ Fluorbritholite-(Y) | (Y,Ca)5(SiO4)3F |
| F | ⓘ Arrheniusite-(Ce) | CaMg[(Ce7Y3)Ca5](SiO4)4(Si2B3AsO18)(BO3)F11 |
| F | ⓘ Åsgruvanite-(Ce) | Ce16Ca5Al(SiO4)6(AsO3)8(CO3)2Cl4F3(OH)2 |
| Mg | Magnesium | |
| Mg | ⓘ Actinolite | ◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2 |
| Mg | ⓘ Cerite-(CeCa) | (Ce7Ca2)◻Mg(SiO4)3(SiO3OH)4(OH)3 |
| Mg | ⓘ Chondrodite | Mg5(SiO4)2F2 |
| Mg | ⓘ Clinohumite | Mg9(SiO4)4F2 |
| Mg | ⓘ Dissakisite-(Ce) | (CaCe)(AlAlMg)O[Si2O7][SiO4](OH) |
| Mg | ⓘ Dollaseite-(Ce) | (CaCe)(MgAlMg)F[Si2O7][SiO4](OH) |
| Mg | ⓘ Dolomite | CaMg(CO3)2 |
| Mg | ⓘ Humite | Mg7(SiO4)3F2 |
| Mg | ⓘ Norbergite | Mg3(SiO4)F2 |
| Mg | ⓘ Phlogopite | KMg3(AlSi3O10)(OH)2 |
| Mg | ⓘ Tremolite | ◻Ca2Mg5(Si8O22)(OH)2 |
| Mg | ⓘ Arrheniusite-(Ce) | CaMg[(Ce7Y3)Ca5](SiO4)4(Si2B3AsO18)(BO3)F11 |
| Al | Aluminium | |
| Al | ⓘ Amphibole Supergroup | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
| Al | ⓘ Dissakisite-(Ce) | (CaCe)(AlAlMg)O[Si2O7][SiO4](OH) |
| Al | ⓘ Dollaseite-(Ce) | (CaCe)(MgAlMg)F[Si2O7][SiO4](OH) |
| Al | ⓘ Phlogopite | KMg3(AlSi3O10)(OH)2 |
| Al | ⓘ Åsgruvanite-(Ce) | Ce16Ca5Al(SiO4)6(AsO3)8(CO3)2Cl4F3(OH)2 |
| Si | Silicon | |
| Si | ⓘ Actinolite | ◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2 |
| Si | ⓘ Amphibole Supergroup | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
| Si | ⓘ Cerite-(CeCa) | (Ce7Ca2)◻Mg(SiO4)3(SiO3OH)4(OH)3 |
| Si | ⓘ Chondrodite | Mg5(SiO4)2F2 |
| Si | ⓘ Clinohumite | Mg9(SiO4)4F2 |
| Si | ⓘ Dissakisite-(Ce) | (CaCe)(AlAlMg)O[Si2O7][SiO4](OH) |
| Si | ⓘ Dollaseite-(Ce) | (CaCe)(MgAlMg)F[Si2O7][SiO4](OH) |
| Si | ⓘ Fluorbritholite-(Ce) | (Ce,Ca)5(SiO4)3F |
| Si | ⓘ Gadolinite-(Ce) | (Ce,La,Nd,Y)2Fe2+Be2Si2O10 |
| Si | ⓘ Gadolinite-(Y) | Y2Fe2+Be2Si2O10 |
| Si | ⓘ Humite | Mg7(SiO4)3F2 |
| Si | ⓘ Norbergite | Mg3(SiO4)F2 |
| Si | ⓘ Phlogopite | KMg3(AlSi3O10)(OH)2 |
| Si | ⓘ Quartz | SiO2 |
| Si | ⓘ Tremolite | ◻Ca2Mg5(Si8O22)(OH)2 |
| Si | ⓘ Fluorbritholite-(Y) | (Y,Ca)5(SiO4)3F |
| Si | ⓘ Allanite Group | (A12+REE3+)(M13+M23+M32+)O[Si2O7][SiO4](OH) |
| Si | ⓘ Arrheniusite-(Ce) | CaMg[(Ce7Y3)Ca5](SiO4)4(Si2B3AsO18)(BO3)F11 |
| Si | ⓘ Åsgruvanite-(Ce) | Ce16Ca5Al(SiO4)6(AsO3)8(CO3)2Cl4F3(OH)2 |
| S | Sulfur | |
| S | ⓘ Bismuthinite | Bi2S3 |
| S | ⓘ Chalcopyrite | CuFeS2 |
| S | ⓘ Molybdenite | MoS2 |
| S | ⓘ Pyrite | FeS2 |
| Cl | Chlorine | |
| Cl | ⓘ Amphibole Supergroup | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
| Cl | ⓘ Åsgruvanite-(Ce) | Ce16Ca5Al(SiO4)6(AsO3)8(CO3)2Cl4F3(OH)2 |
| K | Potassium | |
| K | ⓘ Phlogopite | KMg3(AlSi3O10)(OH)2 |
| Ca | Calcium | |
| Ca | ⓘ Actinolite | ◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2 |
| Ca | ⓘ Calcite | CaCO3 |
| Ca | ⓘ Cerite-(CeCa) | (Ce7Ca2)◻Mg(SiO4)3(SiO3OH)4(OH)3 |
| Ca | ⓘ Dissakisite-(Ce) | (CaCe)(AlAlMg)O[Si2O7][SiO4](OH) |
| Ca | ⓘ Dollaseite-(Ce) | (CaCe)(MgAlMg)F[Si2O7][SiO4](OH) |
| Ca | ⓘ Dolomite | CaMg(CO3)2 |
| Ca | ⓘ Fluorbritholite-(Ce) | (Ce,Ca)5(SiO4)3F |
| Ca | ⓘ Parisite-(Ce) | CaCe2(CO3)3F2 |
| Ca | ⓘ Tremolite | ◻Ca2Mg5(Si8O22)(OH)2 |
| Ca | ⓘ Fluorbritholite-(Y) | (Y,Ca)5(SiO4)3F |
| Ca | ⓘ Arrheniusite-(Ce) | CaMg[(Ce7Y3)Ca5](SiO4)4(Si2B3AsO18)(BO3)F11 |
| Ca | ⓘ Åsgruvanite-(Ce) | Ce16Ca5Al(SiO4)6(AsO3)8(CO3)2Cl4F3(OH)2 |
| Ti | Titanium | |
| Ti | ⓘ Amphibole Supergroup | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
| Fe | Iron | |
| Fe | ⓘ Actinolite | ◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2 |
| Fe | ⓘ Chalcopyrite | CuFeS2 |
| Fe | ⓘ Gadolinite-(Ce) | (Ce,La,Nd,Y)2Fe2+Be2Si2O10 |
| Fe | ⓘ Gadolinite-(Y) | Y2Fe2+Be2Si2O10 |
| Fe | ⓘ Magnetite | Fe2+Fe23+O4 |
| Fe | ⓘ Pyrite | FeS2 |
| Cu | Copper | |
| Cu | ⓘ Chalcopyrite | CuFeS2 |
| As | Arsenic | |
| As | ⓘ Arrheniusite-(Ce) | CaMg[(Ce7Y3)Ca5](SiO4)4(Si2B3AsO18)(BO3)F11 |
| As | ⓘ Åsgruvanite-(Ce) | Ce16Ca5Al(SiO4)6(AsO3)8(CO3)2Cl4F3(OH)2 |
| Y | Yttrium | |
| Y | ⓘ Gadolinite-(Ce) | (Ce,La,Nd,Y)2Fe2+Be2Si2O10 |
| Y | ⓘ Gadolinite-(Y) | Y2Fe2+Be2Si2O10 |
| Y | ⓘ Fluorbritholite-(Y) | (Y,Ca)5(SiO4)3F |
| Y | ⓘ Arrheniusite-(Ce) | CaMg[(Ce7Y3)Ca5](SiO4)4(Si2B3AsO18)(BO3)F11 |
| Mo | Molybdenum | |
| Mo | ⓘ Molybdenite | MoS2 |
| La | Lanthanum | |
| La | ⓘ Gadolinite-(Ce) | (Ce,La,Nd,Y)2Fe2+Be2Si2O10 |
| Ce | Cerium | |
| Ce | ⓘ Bastnäsite-(Ce) | Ce(CO3)F |
| Ce | ⓘ Cerite-(CeCa) | (Ce7Ca2)◻Mg(SiO4)3(SiO3OH)4(OH)3 |
| Ce | ⓘ Dissakisite-(Ce) | (CaCe)(AlAlMg)O[Si2O7][SiO4](OH) |
| Ce | ⓘ Dollaseite-(Ce) | (CaCe)(MgAlMg)F[Si2O7][SiO4](OH) |
| Ce | ⓘ Fluorbritholite-(Ce) | (Ce,Ca)5(SiO4)3F |
| Ce | ⓘ Gadolinite-(Ce) | (Ce,La,Nd,Y)2Fe2+Be2Si2O10 |
| Ce | ⓘ Parisite-(Ce) | CaCe2(CO3)3F2 |
| Ce | ⓘ Arrheniusite-(Ce) | CaMg[(Ce7Y3)Ca5](SiO4)4(Si2B3AsO18)(BO3)F11 |
| Ce | ⓘ Åsgruvanite-(Ce) | Ce16Ca5Al(SiO4)6(AsO3)8(CO3)2Cl4F3(OH)2 |
| Nd | Neodymium | |
| Nd | ⓘ Gadolinite-(Ce) | (Ce,La,Nd,Y)2Fe2+Be2Si2O10 |
| Bi | Bismuth | |
| Bi | ⓘ Bismuthinite | Bi2S3 |
Other Regions, Features and Areas containing this locality
Eurasian PlateTectonic Plate
- Baltic Shield
- Bergslagen-LivoniaShield
EuropeContinent
ScandinaviaRegion
Sweden
- Bergslagen mining districtMining District
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References
Geijer, Per (1926) Norbergite and Fluoborite, two new minerals from the Norberg mining district. Geologiska Föreningen i Stockholm Förhandlingar, 48 (1). 84-85 doi:10.1080/11035892609445642
Geijer, P. (1927) Some mineral associations from the Norberg District. Avhandlingar och uppsatser. Serie C Vol. 20 (4). Sveriges Geologiska Undersökning 32 pp.
Peacor, Donald R., Dunn, Pete J. (1988) Dollaseite-(Ce) (magnesium orthite redefined): Structure refinement and implications for F + M2+ substitutions in epidote-group minerals. American Mineralogist, 73 (7-8) 838-842
Grew, Edward S., Essene, Eric J., Peacor, Donald R., Su, Shu-chun, Asami, Masao (1991) Dissakisite-(Ce), a new member of the epidote group and the Mg analogue of allanite-(Ce), from Antarctica. American Mineralogist, 76 (11-12) 1990-1997
Holtstam, D., Andersson, U. B. (2007) The REE minerals of the Bastnäs-type deposits, South-Central Sweden. The Canadian Mineralogist, 45 (5) 1073-1114 doi:10.2113/gscanmin.45.5.1073
Holtstam, Dan; Bindi, Luca; Bonazzi, Paola; Förster, Hans-Jürgen; Andersson, Ulf B. (2021) Arrheniusite-(Ce), CaMg[(Ce7Y3)Ca5](SiO4)3(Si3B3O18)(AsO4)(BO3)F11, a New Member of the Vicanite Group, from the Östanmossa Mine, Norberg, Sweden. The Canadian Mineralogist, 59 (1). 177-189 doi:10.3749/canmin.2000045






Östanmossa mine, Röberg ore field, Norberg, Västmanland County, Sweden