Hellandite-(Y) (original) (raw)
A valid IMA mineral species
About Hellandite-(Y)Hide
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Formula:
(Ca,REE)4Y2Al◻2(B4Si4O22) (OH)2
In the IMA approved report on hellandites [Am. Mineral.,87 (2002), 745–752], the occupancy at the T sites was given as (Be,Li)2–x, however the value of x was not specified. Actually, it is always x > 1, therefore the T site is vacant in the ideal formula of hellandite-(Y).
Colour:
Nut-brown, brownish red, black, gray, green, yellow, cream, pinkish
Specific Gravity:
2.95 - 3.63
Crystal System:
Monoclinic
Name:
Named in 1903 by Waldemar Christofer Brøgger in honour of Amund Theodor Helland (11 October 1846, Bergen, Norway - 15 November 1918, Kristiania (now Oslo), Norway), professor of geology and geography at the Royal Frederick University (University of Oslo). It was renamed in 1987, but the renaming was not approved until 2002 (IMA Case 00-F). The suffix/modifier indicates the dominant essential REE.
Unique IdentifiersHide
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Long-form identifier:
mindat:1:1:1852:0
4594b406-caeb-4ef4-b239-21e424c76b5a
IMA Classification of Hellandite-(Y)Hide
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IMA status notes:
Redefined by the IMA
IMA Formula:
(Ca,REE)4Y2Al◻2(B4Si4O22)(OH)2
Approval history:
Redefined as hellandite-(Y) by IMA in 2000 (special procedure IMA code 00-F).
Revision of formula: IMA 2017 (CNMNC Newsletter No. 37).
Classification of Hellandite-(Y)Hide
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9.DK.20
9 : SILICATES (Germanates)
D : Inosilicates
K : Inosilicates with 5-periodic single chains
54.2.2.1
54 : NESOSILICATES Borosilicates and Some Beryllosilicates
2 : Borosilicates and Some Beryllosilicates with B in [4] coordination
17.5.51
17 : Silicates Containing other Anions
5 : Borosilicates
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.
Symbol | Source | Reference |
---|---|---|
Hld-Y | IMA–CNMNC | Warr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43 |
Physical Properties of Hellandite-(Y)Hide
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Colour:
Nut-brown, brownish red, black, gray, green, yellow, cream, pinkish
Cleavage:
Poor/Indistinct
Poor on {100}, {010}.
Density:
2.95 - 3.63 g/cm3 (Measured) 3.5(5) g/cm3 (Calculated)
Optical Data of Hellandite-(Y)Hide
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RI values:
_n_α = 1.640 _n_β = 1.650 _n_γ = 1.660
2V:
Measured: 48° to 86°, Calculated: 88°
δ = 0.020
Image shows birefringence interference colour range (at 30µm thickness)
and does not take into account mineral colouration.
Dispersion:
relatively weak
Chemistry of Hellandite-(Y)Hide
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Mindat Formula:
(Ca,REE)4Y2Al◻2(B4Si4O22) (OH)2
In the IMA approved report on hellandites [Am. Mineral.,87 (2002), 745–752], the occupancy at the T sites was given as (Be,Li)2–x, however the value of x was not specified. Actually, it is always x > 1, therefore the T site is vacant in the ideal formula of hellandite-(Y).
Crystallography of Hellandite-(Y)Hide
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Crystal System:
Monoclinic
Class (H-M):
2/m - Prismatic
Cell Parameters:
a = 18.99(1) Å, b = 7.715(5) Å, c = 10.30(1) Å
β = 111.4(1)°
Ratio:
a:b:c = 2.461 : 1 : 1.335
Unit Cell V:
1,404.99 ų (Calculated from Unit Cell)
Twinning:
Contact and polysynthetic, parallel to {001} and {100}.
Crystal StructureHide
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ID | Species | Reference | Link | Year | Locality | Pressure (GPa) | Temp (K) |
---|---|---|---|---|---|---|---|
0000557 | Hellandite-(Y) | Mellini M, Merlino S (1977) Hellandite: a new type of silicoborate chain American Mineralogist 62 89-99 | 1977 | 0 | 293 | ||
0020232 | Hellandite-(Y) | Miyawaki R, Momma K, Yokoyama K, Shigeoka M, Matsubara S, Ito M, Nakai I, Kristiansen R (2015) Mn-bearing hellandite-(Y) from the Heftetjern pegmatite, Tordal, Norway The Canadian Mineralogist 53 345-356 | 2015 | Heftetjern, Tordal, Telemark, Norway | 0 | 293 |
CIF Raw Data - click here to close
X-Ray Powder DiffractionHide
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Powder Diffraction Data:
d-spacing | Intensity |
---|---|
2.812 Å | (100) |
4.69 Å | (80) |
2.635 Å | (80) |
2.603 Å | (80) |
3.436 Å | (70) |
3.198 Å | (70) |
3.068 Å | (70) |
Geological EnvironmentHide
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Type Occurrence of Hellandite-(Y)Hide
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Place of Conservation of Type Material:
Mineralogical-Geological Museum, University of Oslo, Oslo, Norway, numbers 21846, various (cotype).
Muséum Nationale d’Histoire Naturelle, Paris, France, number 109732 (type).
Associated Minerals at Type Locality:
Synonyms of Hellandite-(Y)Hide
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Other Language Names for Hellandite-(Y)Hide
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Varieties of Hellandite-(Y)Hide
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Relationship of Hellandite-(Y) to other SpeciesHide
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Other Members of this group:
Structurally related to group(s):
Common AssociatesHide
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Associated Minerals Based on Photo Data:
Related Minerals - Strunz-mindat GroupingHide
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9.DK. | Ferrorhodonite | CaMn3Fe[Si5O15] | Tric. 1 : _P_1 |
---|---|---|---|
9.DK. | Vittinkiite | MnMn3Mn[Si5O15] | Tric. 1 : _P_1 |
9.DK. | Ferri-hellandite-(Ce) | (Ca3Ce)Ce2Fe3+◻2B4Si4O22(OH)2 | Mon. 2/m : _P_2/b |
9.DK. | Shijiangshanite | Pb3CaAl(Si5O14)(OH)3 · 3H2O | Trig. 3_m_ : R_3_c |
9.DK.05 | Allagite | ||
9.DK.05 | Babingtonite | Ca2(Fe,Mn)FeSi5O14(OH) | Tric. 1 : _P_1 |
9.DK.05 | Lithiomarsturite | LiCaMn3Si5O14(OH) | Tric. 1 : _P_1 |
9.DK.05 | Manganbabingtonite | Ca2(Mn,Fe)FeSi5O14(OH) | Tric. 1 : _P_1 |
9.DK.05 | Marsturite | NaCaMn3Si5O14(OH) | Tric. 1 : _P_1 |
9.DK.05 | Nambulite | LiMn2+4Si5O14(OH) | Tric. |
9.DK.05 | Natronambulite | (Na,Li)(Mn,Ca)4Si5O14OH | Tric. |
9.DK.05 | Rhodonite | CaMn3Mn[Si5O15] | Tric. 1 |
9.DK.05 | Scandiobabingtonite | Ca2(Fe2+,Mn)ScSi5O14(OH) | Tric. |
9.DK.10 | Santaclaraite | CaMn4[Si5O14OH](OH) · H2O | Tric. 1 : _P_1 |
9.DK.15 | Saneroite | NaMn2+5[Si5O14(OH)](VO3)(OH) | Tric. 1 : _P_1 |
9.DK.20 | Tadzhikite-(Ce) | Ca4Ce3+2Ti◻2(B4Si4O22)(OH)2 | Mon. 2/m : _P_2/b |
9.DK.20 | Hellandite-(Yb) | (Ca,Y)4(Yb,Y)2(Al,Fe3+,Ti4+)(Be,Li)2[B4Si4O22](O,F,OH)2 | |
9.DK.20 | Mottanaite-(Ce) | Ca4(Ce,REE)Σ2Al(Be1.5◻0.5)Σ2[B4Si4O22]O2 | Mon. 2/m |
9.DK.20 | Ciprianiite | Ca4[(Th,U),Ca]Σ2Al(Be0.5◻1.5)Σ2[B4Si4O22](OH)2 | Mon. 2/m : _P_2/b |
9.DK.20 | Hellandite-(Ce) | (Ca,REE)4Ce2Al◻2(B4Si4O22) (OH)2 | Mon. 2/m |
9.DK.20 | Ferri-mottanaite-(Ce) | Ca4Ce2Fe3+(Be1.5◻0.5)[Si4B4O22]O2 | Mon. 2/m : _P_2/b |
Other InformationHide
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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 Hellandite-(Y)Hide
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References for Hellandite-(Y)Hide
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Reference List:
Oberti, Roberta, Ventura, Giancarlo Della, Ottolini, Luisa, Hawthorne, Frank C., Bonazzi, Paola (2002) Re-definition, nomenclature and crystal-chemistry of the hellandite group. American Mineralogist, 87 (5) 745-752 doi:10.2138/am-2002-5-618
Miyawaki, Ritsuro, Momma, Koichi, Yokoyama, Kazumi, Shigeoka, Masako, Matsubara, Satoshi, Ito, Miku, Nakai, Izumi, Kristiansen, Roy (2015) Mn-bearing hellandite-(Y) from Heftetjern pegmatite, Tørdal, Norway. The Canadian Mineralogist, 53 (2) 345-356 doi:10.3749/canmin.1400068
Ondrejka, Martin, Molnárová, Alexandra, Putiš, Marián, Bačík, Peter, Uher, Pavel, Voleková, Bronislava, Milovská, Stanislava, Mikuš, Tomáš, Pukančík, Libor (2022) Hellandite-(Y)–hingganite-(Y)–fluorapatite retrograde coronae: a novel type of fluid-induced dissolution–reprecipitation breakdown of xenotime-(Y) in the metagranites of Fabova Hoľa, Western Carpathians, Slovakia. Mineralogical Magazine, 86 (4) 586-605 doi:10.1180/mgm.2022.7
Localities for Hellandite-(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.