Britholite-(Y) (original) (raw)
A valid IMA mineral species - grandfathered
About Britholite-(Y)Hide
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Colour:
Reddish-brown, black
Lustre:
Adamantine, Resinous, Dull
Name:
First described as abukumalite by Hata (1938) from the Suishoyama pegmatite, Fukushima Prefecture, Japan. Later it was renamed as britholite-(Y) as part of the changes in nomenclature for rare-earth minerals (Levinson 1966). It is named for its relation to britholite-(Ce) and the suffix "-(Y)" due to the dominance of yttrium in the composition.
Unique IdentifiersHide
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Long-form identifier:
mindat:1:1:776:2
970d464d-1b07-496d-90bb-6df34a3fee99
IMA Classification of Britholite-(Y)Hide
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Approved, 'Grandfathered' (first described prior to 1959)
IMA status notes:
Renamed by the IMA
IMA Formula:
(Y,Ca)5(SiO4)3(OH)
Classification of Britholite-(Y)Hide
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9.AH.25
9 : SILICATES (Germanates)
A : Nesosilicates
H : Nesosilicates with CO3, SO4, PO4, etc.
52.4.9.2
52 : NESOSILICATES Insular SiO4 Groups and O,OH,F,H2O
4 : Insular SiO4 Groups and O, OH, F, and H2O with cations in [6] and/or >[6] coordination
17.6.16
17 : Silicates Containing other Anions
6 : Silicates with phosphate
Mineral SymbolsHide
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As of 2021 there are now IMA–CNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.
Please only use the official IMA–CNMNC symbol. Older variants are listed for historical use only.
Symbol | Source | Reference |
---|---|---|
Bri-Y | IMA–CNMNC | Warr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43 |
Bri | The Canadian Mineralogist (2019) | The Canadian Mineralogist (2019) The Canadian Mineralogist list of symbols for rock- and ore-forming minerals (December 30, 2019). download |
Physical Properties of Britholite-(Y)Hide
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Adamantine, Resinous, Dull
Transparency:
Transparent, Translucent
Colour:
Reddish-brown, black
Comment:
Yellowish-brown in thin sections.
Cleavage:
Imperfect/Fair
Imperfect on {0001}, {1010}.
Fracture:
Irregular/Uneven, Splintery
Density:
4.35 g/cm3 (Measured) 4.44 g/cm3 (Calculated)
Optical Data of Britholite-(Y)Hide
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RI values:
_n_ω = 1.730 - 1.752 _n_ε = 1.728 - 1.750
δ = 0.002
Image shows birefringence interference colour range (at 30µm thickness)
and does not take into account mineral colouration.
Optical Extinction:
Parallel to cleavage.
Chemistry of Britholite-(Y)Hide
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Mindat Formula:
(Y,Ca)5(SiO4)3OH
Crystallography of Britholite-(Y)Hide
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Class (H-M):
6/m - Dipyramidal
Cell Parameters:
a = 9.43 Å, c = 6.81 Å
Unit Cell V:
524.45 ų (Calculated from Unit Cell)
Crystal StructureHide
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ID | Species | Reference | Link | Year | Locality | Pressure (GPa) | Temp (K) |
---|---|---|---|---|---|---|---|
0011044 | Britholite-(Y) | Noe D C, Hughes J M, Mariano A N, Drexler J W, Kato A (1993) The crystal structure of monoclinic britholite-(Ce) and britholite-(Y) Zeitschrift fur Kristallographie 206 233-246 | 1993 | Suishoyama, Japan | 0 | 293 | |
0011045 | Britholite-(Y) | Noe D C, Hughes J M, Mariano A N, Drexler J W, Kato A (1993) The crystal structure of monoclinic britholite-(Ce) and britholite-(Y) Zeitschrift fur Kristallographie 206 233-246 | 1993 | Suishoyama, Japan | 0 | 293 |
CIF Raw Data - click here to close
X-Ray Powder DiffractionHide
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Powder Diffraction Data:
d-spacing | Intensity |
---|---|
2.813 Å | (100) |
2.753 Å | (90) |
2.727 Å | (80) |
3.13 Å | (50) |
3.09 Å | (50) |
3.39 Å | (30) |
1.885 Å | (30) |
Comments:
Suishoyama pegmatite, Japan.
Geological EnvironmentHide
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Type Occurrence of Britholite-(Y)Hide
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General Appearance of Type Material:
Massive, measuring about 1-2 cm in diameter. Rarely as short prismatic crystals to 3 cm. The outer part of the mineral is always altered into earthy substance of yellowish white or yellowish brown color.
Place of Conservation of Type Material:
Type material destroyed in WWII.
Geological Setting of Type Material:
Associated Minerals at Type Locality:
Synonyms of Britholite-(Y)Hide
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Other Language Names for Britholite-(Y)Hide
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Relationship of Britholite-(Y) to other SpeciesHide
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Other Members of this group:
Britholite-(Ce) | (Ce,Ca)5(SiO4)3OH | Hex. 6/m : _P_63/m |
---|---|---|
Britholite-(La) | Ca2(La,Ce,Ca)3(SiO4,PO4)3(OH,F) | |
Calciobritholite | (Ca,Y)5(SiO4,PO4)3(OH) | |
Fluorbritholite-(Ce) | (Ce,Ca)5(SiO4)3F | Hex. 6/m : _P_63/m |
Fluorbritholite-(Nd) | Ca2Nd3(SiO4)3F | Hex. 6/m : _P_63/m |
Fluorbritholite-(Y) | (Y,Ca)5(SiO4)3F | Hex. 6/m : _P_63/m |
Fluorcalciobritholite | (Ca,REE)5(SiO4,PO4)3F | Hex. 6/m : _P_63/m |
Tritomite-(Ce) | Ce5(SiO4,BO4)3(OH,O) | |
Tritomite-(Y) | Y5(SiO4,BO4)3(O,OH,F) |
Common AssociatesHide
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Associated Minerals Based on Photo Data:
Related Minerals - Strunz-mindat GroupingHide
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9.AH. | Fluorbritholite-(Nd) | Ca2Nd3(SiO4)3F | Hex. 6/m : _P_63/m |
---|---|---|---|
9.AH.05 | Iimoriite-(Y) | Y2[SiO4][CO3] | Tric. 1 : _P_1 |
9.AH.10 | Tundrite-(Ce) | Na2Ce2Ti(SiO4)(CO3)2O2 | Tric. 1 : _P_1 |
9.AH.10 | Tundrite-(Nd) | Na2(Nd,Ce)2Ti(SiO4)(CO3)2O2 | |
9.AH.15 | Spurrite | Ca5(SiO4)2(CO3) | Mon. 2/m : _P_21/b |
9.AH.15 | Galuskinite | Ca7(SiO4)3(CO3) | Mon. 2/m : _P_21/b |
9.AH.20 | Ternesite | Ca5(SiO4)2(SO4) | Orth. m m m _(_2/_m_2/_m_2/m ) : P n m a |
9.AH.20 | Silicocarnotite | Ca5[(SiO4)(PO4)](PO4) | Orth. m m m _(_2/_m_2/_m_2/m ) : P n m a |
9.AH.25 | Britholite-(Ce) | (Ce,Ca)5(SiO4)3OH | Hex. 6/m : _P_63/m |
9.AH.25 | Chlorellestadite | Ca5(SiO4)1.5(SO4)1.5Cl | Hex. 6/m : _P_63/m |
9.AH.25 | Fluorbritholite-(Ce) | (Ce,Ca)5(SiO4)3F | Hex. 6/m : _P_63/m |
9.AH.25 | Fluorellestadite | Ca5(SiO4)1.5(SO4)1.5F | Hex. 6/m : _P_63/m |
9.AH.25 | Hydroxylellestadite | Ca5(SiO4)1.5(SO4)1.5(OH) | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_63/m c m |
9.AH.25 | Mattheddleite | Pb5(SiO4)1.5(SO4)1.5(Cl,OH) | Hex. 6/m : _P_63/m |
9.AH.25 | Tritomite-(Ce) | Ce5(SiO4,BO4)3(OH,O) | |
9.AH.25 | Tritomite-(Y) | Y5(SiO4,BO4)3(O,OH,F) | |
9.AH.25 | Fluorcalciobritholite | (Ca,REE)5(SiO4,PO4)3F | Hex. 6/m : _P_63/m |
9.AH.25 | Fluorbritholite-(Y) | (Y,Ca)5(SiO4)3F | Hex. 6/m : _P_63/m |
9.AH.25 | Britholite-(La) | Ca2(La,Ce,Ca)3(SiO4,PO4)3(OH,F) | |
9.AH.25 | Calciobritholite | (Ca,Y)5(SiO4,PO4)3(OH) | |
9.AH.35 | Nabimusaite | KCa12(SiO4)4(SO4)2O2F | Trig. 3_m_ _(_32/m ) : R_3_m |
9.AH.35 | Dargaite | BaCa12(SiO4)4(SO4)2O3 | Trig. 3_m_ : R_3_m |
9.AH.40 | Zadovite | BaCa6[(SiO4)(PO4)](PO4)2F | Trig. 3_m_ : R_3_m |
9.AH.40 | Gazeevite | BaCa6(SiO4)2(SO4)2O | Trig. 3_m_ _(_32/m ) : R_3_m |
9.AH.40 | Stracherite | BaCa6(SiO4)2[(PO4)(CO3)]2F | Trig. 3_m_ _(_32/m ) : R_3_m |
9.AH.45 | Flamite | Ca8-x(Na,K)x(SiO4)4-x(PO4)x | Orth. m _m_2 |
9.AH.50 | Byzantievite | Ba5(Ca,REE,Y)22(Ti,Nb)18(SiO4)4[(PO4),(SiO4)]4(BO3)9O22[(OH),F]43(H2O)1.5 | Trig. 3 : _R_3 |
9.AH.55 | Greenwoodite | (Ba,V3+O)2V3+9(Fe3+,Fe2+)2Si2O22 | Trig. 3_m_ _(_32/m ) : _P_3_m_1 |
9.AH.60 | Kihlmanite-(Ce) | Ce2TiO2(SiO4)(HCO3)2(H2O) | Tric. 1 : _P_1 |
9.AH.65 | Tsangpoite | Ca5(PO4)2(SiO4) | Hex. |
9.AH.70 | Enalite | (Th,REE,Al) [(PO4),(SiO4),(OH)] | Tet. |
Other InformationHide
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Notes:
Readily dissolved in cold dilute mineral acids.
Magnetic property is weaker than allanite and greater than yttrialite and xenotime.
Health Risks:
No information on health risks for this material has been entered into the database. You should always treat mineral specimens with care.
Internet Links for Britholite-(Y)Hide
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References for Britholite-(Y)Hide
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Localities for Britholite-(Y)Hide
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This map shows a selection of localities that have latitude and longitude coordinates recorded. Click on the symbol to view information about a locality. The symbol next to localities in the list can be used to jump to that position on the map.
Locality ListHide
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- This locality has map coordinates listed. - This locality has estimated coordinates. ⓘ - Click for references and further information on this occurrence. ? - Indicates mineral may be doubtful at this locality. - Good crystals or important locality for species. - World class for species or very significant. (TL) - Type Locality for a valid mineral species. (FRL) - First Recorded Locality for everything else (eg varieties). Struck out - Mineral was erroneously reported from this locality. Faded * - Never found at this locality but inferred to have existed at some point in the past (e.g. from pseudomorphs).
All localities listed without proper references should be considered as questionable.