Låvenite
A valid IMA mineral species - grandfathered
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About Låvenite
Formula:
Na2Ca2Mn2Zr2(Si2O7)2O2F2
Formula from Dal Bo et al. (2022).
Colour:
Colorless to brownish-yellow, brown, brownish-red, orange-brown.
Lustre:
Vitreous, Greasy
Hardness:
6
Specific Gravity:
3.4 - 3.55
Crystal System:
Monoclinic
Member of:
Name:
Named for the type locality, Låven island, Langesundsfjord, Norway by the Norwegian geologist and mineralogist Waldemar Christopher Brøgger (10 November 1851 – 17 February 1940). In 1875, Brøgger and Hans Reusch had found, in a nepheline syenite pegmatite at Låven, a mineral first assumed by Brøgger to be mosandrite (Brøgger 1878). Later he recognized it as a new mineral and gave a preliminary description (Brøgger 1885).
A more detailed description was published by Brøgger (1890). The crystal structure was solved by Mellini (1981) and refined on samples from Lovozero, Russia by Simenov and Belov (1960) and from Los Archipelago, Guinea by Biagoni et al. (2012).
Dal Bo et al. (2022) reviewed the data on låvenite in their paper on the wöhlerite group minerals.
A more detailed description was published by Brøgger (1890). The crystal structure was solved by Mellini (1981) and refined on samples from Lovozero, Russia by Simenov and Belov (1960) and from Los Archipelago, Guinea by Biagoni et al. (2012).
Dal Bo et al. (2022) reviewed the data on låvenite in their paper on the wöhlerite group minerals.
Type Locality:
Isostructural with:
A sorosilicate belonging to the wöhlerite group. Forms a solid solution-series with normandite, where låvenite is the Zr- and normandite the Ti-endmember.
May be the Mn analogue of UM2003-34-SiO:CaFFeMnNaNbTiZr; and also the Mn analogue of madeiraite (?).
The structure of Låvenite structure can be described as four-columns wide "octahedral" walls interconnected by corner-sharing and via disilicate groups. Structural and chemical data indicate cationic substitution on the four X sites. X2 and X4, which are the largest sites in the "octahedral" wall, are dominated by Ca and Na, respectively. The site X3 is dominated by Mn2+ and X1, the smallest site, is dominated by Zr (Dal Bo et al. 2022)
May be the Mn analogue of UM2003-34-SiO:CaFFeMnNaNbTiZr; and also the Mn analogue of madeiraite (?).
The structure of Låvenite structure can be described as four-columns wide "octahedral" walls interconnected by corner-sharing and via disilicate groups. Structural and chemical data indicate cationic substitution on the four X sites. X2 and X4, which are the largest sites in the "octahedral" wall, are dominated by Ca and Na, respectively. The site X3 is dominated by Mn2+ and X1, the smallest site, is dominated by Zr (Dal Bo et al. 2022)
Name Encoding
ASCII-7:
Lavenite
Unique Identifiers
Mindat ID:
2462
Long-form identifier:
mindat:1:1:2462:0
Similar Names
IMA Classification of Låvenite
Approved, 'Grandfathered' (first described prior to 1959)
IMA Formula:
(Na,Ca)2(Mn2+,Fe2+)(Zr4+,Ti4+,Nb5+)(Si2O7)(O,F)2
First published:
1885
Classification of Låvenite
9.BE.17
9 : SILICATES (Germanates)
B : Sorosilicates
E : Si2O7 groups, with additional anions; cations in octahedral [6] and greater coordination
9 : SILICATES (Germanates)
B : Sorosilicates
E : Si2O7 groups, with additional anions; cations in octahedral [6] and greater coordination
Dana 7th ed.:
56.2.4.4
56.2.4.4
56 : SOROSILICATES Si2O7 Groups, With Additional O, OH, F and H2O
2 : Si2O7 Groups and O, OH, F, and H2O with cations in [4] and/or >[4] coordination
56 : SOROSILICATES Si2O7 Groups, With Additional O, OH, F and H2O
2 : Si2O7 Groups and O, OH, F, and H2O with cations in [4] and/or >[4] coordination
14.10.27
14 : Silicates not Containing Aluminum
10 : Silicates of Zr or Hf
14 : Silicates not Containing Aluminum
10 : Silicates of Zr or Hf
Mineral Symbols
As of 2021 there are now IMA–CNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.
| Symbol | Source | Reference for Standard |
|---|---|---|
| Låv | 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 Låvenite
Vitreous, Greasy
Transparency:
Transparent, Translucent
Colour:
Colorless to brownish-yellow, brown, brownish-red, orange-brown.
Streak:
Yellowish-white; pale brown
Hardness:
6 on Mohs scale
Tenacity:
Brittle
Cleavage:
Distinct/Good
Good on {100}
Good on {100}
Fracture:
Irregular/Uneven
Density:
3.4 - 3.55 g/cm3 (Measured) 3.498 g/cm3 (Calculated)
Optical Data of Låvenite
Type:
Biaxial (-)
RI values:
nα = 1.67 nβ = 1.69 nγ = 1.72
2V:
Measured: 40° to 70°, Calculated: 80°
Max. Birefringence:
δ = 0.050
Based on recorded range of RI values above.
Based on recorded range of RI values above.
Interference Colours:
The colours simulate birefringence patterns seen in thin section under crossed polars. They do not take into account mineral colouration or opacity.
Michel-Levy Bar The default colours simulate the birefringence range for a 30 µm thin-section thickness. Adjust the slider to simulate a different thickness.
Grain Simulation You can rotate the grain simulation to show how this range might look as you rotated a sample under crossed polars. Each grain retains its interference colour (retardation) while its brightness falls to black at extinction and reaches a maximum between extinction positions.
The colours simulate birefringence patterns seen in thin section under crossed polars. They do not take into account mineral colouration or opacity.
Michel-Levy Bar The default colours simulate the birefringence range for a 30 µm thin-section thickness. Adjust the slider to simulate a different thickness.
Grain Simulation You can rotate the grain simulation to show how this range might look as you rotated a sample under crossed polars. Each grain retains its interference colour (retardation) while its brightness falls to black at extinction and reaches a maximum between extinction positions.
Surface Relief:
Very High (positive)
Relative to Canada balsam mounting medium (n ≈ 1.537).
Relative to Canada balsam mounting medium (n ≈ 1.537).
This shows the grain boundary and Becke line effect under plane-polarised
light, based on the contrast between this mineral's average refractive
index and the mounting medium. It does not take into account mineral
colouration.
In focus
Interference Figure:
This shows the idealized biaxial acute bisectrix (Bxa) interference figure
- the conoscopic view for a grain cut perpendicular to the acute bisectrix, using
this mineral's 2V. The two small white dots mark the melatopes - the points
where the two optic axes emerge - and are shown only when they fall within the
field of view. The coloured bands are isochromatics, and the dark bands are
isogyres.
Rotate the stage: at 0°/90° the isogyres form a cross through the melatopes; at 45° they pull apart into curved hyperbolas. That splitting on rotation - absent in a uniaxial figure - is the standard diagnostic test for telling biaxial minerals from uniaxial ones. If 2V is large, the melatopes may fall outside the field of view, as they often do at the microscope too.
Rotate the stage: at 0°/90° the isogyres form a cross through the melatopes; at 45° they pull apart into curved hyperbolas. That splitting on rotation - absent in a uniaxial figure - is the standard diagnostic test for telling biaxial minerals from uniaxial ones. If 2V is large, the melatopes may fall outside the field of view, as they often do at the microscope too.
Dispersion:
r < v perceptible
Optical Extinction:
Y = b; Z ∧ c = -20°.
Pleochroism:
Visible
Comments:
X = colorless, pale yellow; Y = colorless, pale greenish yellow; Z = very pale yellow, orange to brownish yellow.
Comments:
Absorption: Z > Y > X.
Chemistry of Låvenite
Mindat Formula:
Na2Ca2Mn2Zr2(Si2O7)2O2F2
Formula from Dal Bo et al. (2022).
Formula from Dal Bo et al. (2022).
Element Weights:
Chemical Analysis
Oxide wt%:
| 1 | 2 | 3 | 4 | |
|---|---|---|---|---|
| SiO2 | 29.63 % | 26.93 % | 28.9 % | 29.72 % |
| TiO2 | 2.35 % | 4.30 % | 3.2 % | 3.22 % |
| ZrO2 | 28.79 % | 21.70 % | 27.2 % | 27.40 % |
| Fe2O3 | 4.73 % | |||
| (Nb, Ta)2O5 | 5.20 % | |||
| MnO | 5.59 % | 11.66 % | 5.3 % | 5.54 % |
| CaO | 9.70 % | 7.74 % | 8.2 % | 8.32 % |
| Na2O | 10.77 % | 10.59 % | 11.9 % | 12.44 % |
| LOI | 2.24 % | |||
| Nb2O5 | 6.10 % | 6.0 % | 4.73 % | |
| HfO2 | 0.36 % | 0.7 % | ||
| ThO2 | 0.03 % | |||
| Y2O3 | 0.19 % | 0.83 % | 0.23 % | |
| Ce2O3 | 0.06 % | |||
| Pr2O3 | 0.04 % | |||
| Nd2O3 | 0.03 % | |||
| Sm2O3 | 0.12 % | |||
| Gd2O3 | 0.09 % | |||
| Dy2O3 | 0.07 % | |||
| Er2O3 | 0.06 % | |||
| Yb2O3 | 0.06 % | |||
| MgO | 0.09 % | 0.11 % | 0.12 % | |
| FeO | 2.48 % | 3.6 % | 3.86 % | |
| F | 5.60 % | 3.44 % | 4.68 % | |
| O=F | -2.36 % | -1.45 % | -1.97 % | |
| Al2O3 | 0.02 % | |||
| Ta2O5 | 0.2 % | |||
| REE2O3 | 0.47 % | |||
| Total: | 99 % | 95.94 % | 98.62 % | 98.29 % |
Sample references:
| ID | Locality | Reference | Notes |
|---|---|---|---|
| 1 | Natrolittodden, Vesle Arøya, Larvik Commune, Vestfold, Norway | wet-chemical analysis by Cleve | |
| 2 | Los Archipelago, Conakry Region, Guinea | Electron microprobe | |
| 3 | Natrolittodden, Vesle Arøya, Larvik Commune, Vestfold, Norway | EMPA + ICPMS data. 5mm brown, elongated crystal | |
| 4 | Langesundsfjorden, Norway | electron microprobe |
Crystallography of Låvenite
Crystal System:
Monoclinic
Class (H-M):
2/m - Prismatic
Space Group:
P21/c
Setting:
P21/a
Cell Parameters:
a = 10.83(1) Å, b = 9.98(1) Å, c = 7.174(5) Å
β = 108.1°
β = 108.1°
Ratio:
a:b:c = 1.085 : 1 : 0.719
Unit Cell V:
737.02 ų (Calculated from Unit Cell)
Z:
4
Morphology:
Crystals prismatic parallel to [100] or tabular. Also acicular radial, fibrous, granular, or massive. Forms include {100}, {110}, {111}, {101}.
Twinning:
Polysynthetic on {100}.
X-Ray Powder Diffraction
Powder Diffraction Data:
| d-spacing | Intensity |
|---|---|
| 3.97 Å | (50) |
| 3.21 Å | (70) |
| 2.89 Å | (100) |
| 2.82 Å | (90) |
| 2.00 Å | (50) |
| 1.792 Å | (50) |
| 1.649 Å | (40) |
Geological Environment
Paragenetic Mode(s):
| Paragenetic Mode | Earliest Age (Ga) |
|---|---|
| Stage 4b: Highly evolved igneous rocks | >3.0 |
| 35 : Ultra-alkali and agpaitic igneous rocks |
Type Occurrence of Låvenite
General Appearance of Type Material:
Chest-nut brown to yellow elongated, prismatic crystals.
Place of Conservation of Type Material:
Naturhistoriska Riksmuseet, Stockholm, Sweden inventory nr. 531056
Geological Setting of Type Material:
nepheline syenite pegmatite
Associated Minerals at Type Locality:
Synonyms of Låvenite
Other Language Names for Låvenite
Varieties of Låvenite
| Titan-låvenite | A name used by petrologists, but mineralogically a titanium-rich låvenite. |
Relationship of Låvenite to other Species
Member of:
Other Members of Wöhlerite Group:
| Baghdadite | Ca6Zr2(Si2O7)2O4 | Mon. 2/m : P21/c |
| Burpalite | Na2CaZr(Si2O7)F2 | Mon. 2/m : P21/c |
| Cuspidine | Ca8(Si2O7)2F4 | Mon. 2/m : P21/c |
| Hiortdahlite | Na2Ca4(Ca0.5Zr0.5)Zr(Si2O7)2OF3 | Tric. 1 : P1 |
| Janhaugite | (Na,Ca)3(Mn2+,Fe2+)3(Ti,Zr,Nb)2(Si2O7)2O2(OH,F)2 | Mon. 2/m : P21/m |
| Madeiraite | Na2Ca2Fe2Zr2(Si2O7)2O2F2 | Mon. 2/m : P21/c |
| Moxuanxueite | NaCa6Zr(Si2O7)2OF3 | Tric. 1 : P1 |
| Niocalite | (Ca,Nb)4(Si2O7)(O,OH,F)2 | Mon. m |
| Normandite | NaCa(Mn,Fe)(Ti,Nb,Zr)(Si2O7)OF | Mon. 2/m : P21/c |
| Pilanesbergite | Na2Ca2Fe2Ti2(Si2O7)2O2F2 | Mon. 2/m : P21/c |
| Wöhlerite | Na2Ca4ZrNb(Si2O7)2O3F | Mon. 2 : P21 |
Common Associates
Associations Based on Photo Data:
| 50 photos of Låvenite associated with Wöhlerite | Na2Ca4ZrNb(Si2O7)2O3F |
| 17 photos of Låvenite associated with Sanidine | K(AlSi3O8) |
| 14 photos of Låvenite associated with Augite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| 13 photos of Låvenite associated with Microcline | K(AlSi3O8) |
| 10 photos of Låvenite associated with Aegirine | NaFe3+Si2O6 |
| 9 photos of Låvenite associated with Kupletskite Group | |
| 8 photos of Låvenite associated with Astrophyllite | K2NaFe2+7Ti2[Si4O12]2O2(OH)4F |
| 6 photos of Låvenite associated with Pyroxene Group | ADSi2O6 |
| 6 photos of Låvenite associated with Albite | Na(AlSi3O8) |
| 5 photos of Låvenite associated with Phlogopite | KMg3(AlSi3O10)(OH)2 |
Related Minerals - Strunz-mindat Grouping
| 9.BE. | Zinkgruvanite | Ba4Mn2+4Fe3+2(Si2O7)2(SO4)2O2(OH)2 |
| 9.BE. | Calciomurmanite | (Na,◻)2Ca(Ti,Mg,Nb)4[Si2O7]2O2(OH,O)2(H2O)4 |
| 9.BE. | Cámaraite | Ba3Na(Fe2+,Mn)8Ti4(Si2O7)4O4(OH,F)7 |
| 9.BE. | Alfredcasparite | Sr2TiO(Si2O7) |
| 9.BE. | Batievaite-(Y) | Y2Ca2Ti(Si2O7)2(OH)2(H2O)4 |
| 9.BE. | Nacareniobsite-(Y) | Na3Ca3YNb(Si2O7)2OF3 |
| 9.BE. | Alexkuznetsovite-(Ce) | Ce2Mn(CO3)(Si2O7) |
| 9.BE. | Bobshannonite | Na2KBa(Mn,Na)8(Nb,Ti)4(Si2O7)4O4(OH)4(O,F)2 |
| 9.BE. | Paralomonosovite | Na6◻4Ti4(Si2O7)2[PO3OH][PO2(OH)2]O2(OF) |
| 9.BE. | Madeiraite | Na2Ca2Fe2Zr2(Si2O7)2O2F2 |
| 9.BE. | Bortolanite | Ca2(Ca1.5Zr0.5)Na(NaCa)Ti(Si2O7)2(OF)F2 |
| 9.BE. | Longshoushanite-(Ce) | Ce4MgAl2Ti2(Si2O7)2O8 |
| 9.BE. | Moxuanxueite | NaCa6Zr(Si2O7)2OF3 |
| 9.BE. | Delhuyarite-(Ce) | Ce4Mg(Fe3+,W)3◻(Si2O7)2O6(OH)2 |
| 9.BE. | Christofschäferite-(Ce) | Ce3CaMnTiFe3+Ti2(Si2O7)2O8 |
| 9.BE.X | Asimowite | Fe2+4O(Si2O7) |
| 9.BE. | Biraite-(La) | La2Fe2+(CO3)(Si2O7) |
| 9.BE. | Pilanesbergite | Na2Ca2Fe2Ti2(Si2O7)2O2F2 |
| 9.BE.02 | Wadsleyite | Mg4O(Si2O7) |
| 9.BE.02 | Ohtaniite | Mg3(Si0.5◻0.5)Si2O8 |
| 9.BE.05 | Lawsonite | CaAl2(Si2O7)(OH)2 · H2O |
| 9.BE.05 | Hennomartinite | SrMn3+2(Si2O7)(OH)2 · H2O |
| 9.BE.05 | Cortesognoite | CaV2(Si2O7)(OH)2 · H2O |
| 9.BE.05 | Noelbensonite | BaMn3+2(Si2O7)(OH)2 · H2O |
| 9.BE.05 | Itoigawaite | SrAl2(Si2O7)(OH)2 · H2O |
| 9.BE.07 | Ilvaite | CaFe3+Fe2+2(Si2O7)O(OH) |
| 9.BE.07 | Amamoorite | CaMn2+2Mn3+(Si2O7)O(OH) |
| 9.BE.07 | Manganilvaite | CaFe2+Fe3+Mn2+(Si2O7)O(OH) |
| 9.BE.10 | Suolunite | Ca2(H2Si2O7) · H2O |
| 9.BE.12 | Jaffeite | Ca6(Si2O7)(OH)6 |
| 9.BE.15 | Fresnoite | Ba2Ti(Si2O7)O |
| 9.BE.17 | Janhaugite | (Na,Ca)3(Mn2+,Fe2+)3(Ti,Zr,Nb)2(Si2O7)2O2(OH,F)2 |
| 9.BE.17 | Burpalite | Na2CaZr(Si2O7)F2 |
| 9.BE.17 | Niocalite | (Ca,Nb)4(Si2O7)(O,OH,F)2 |
| 9.BE.17 | Normandite | NaCa(Mn,Fe)(Ti,Nb,Zr)(Si2O7)OF |
| 9.BE.17 | Hiortdahlite | Na2Ca4(Ca0.5Zr0.5)Zr(Si2O7)2OF3 |
| 9.BE.17 | Cuspidine | Ca8(Si2O7)2F4 |
| 9.BE.17 | Wöhlerite | Na2Ca4ZrNb(Si2O7)2O3F |
| 9.BE.17 | Baghdadite | Ca6Zr2(Si2O7)2O4 |
| 9.BE.20 | Nacareniobsite-(Ce) | Na3Ca3(Ce,REE)Nb(Si2O7)2OF3 |
| 9.BE.20 | Roumaite | (Ca,Na,REE,◻)7(Nb,Ti)[Si2O7]2OF3 |
| 9.BE.20 | Rinkite-(Ce) | (Ca3Ce)Na(NaCa)Ti(Si2O7)2(OF)F2 |
| 9.BE.20 | Nacareniobsite-(Nd) | Ca2(CaNd)Na3Nb(Si2O7)2(OF)F2 |
| 9.BE.20 | Rinkite-(Y) | Na2Ca4YTi(Si2O7)2OF3 |
| 9.BE.20 | Mosandrite-(Ce) | (Ca3REE)[(H2O)2Ca0.5◻0.5]Ti(Si2O7)2(OH)2(H2O)2 |
| 9.BE.22 | Hainite-(Y) | Na2Ca4(Y,REE)Ti(Si2O7)2OF3 |
| 9.BE.22 | Rosenbuschite | Na6Ca6Zr3Ti(Si2O7)4O2F6 |
| 9.BE.22 | Götzenite | NaCa6Ti(Si2O7)2OF3 |
| 9.BE.22 | Fogoite-(Y) | Na3Ca2Y2Ti(Si2O7)2OF3 |
| 9.BE.22 | Kochite | Na3Ca2MnZrTi(Si2O7)2OF3 |
| 9.BE.23 | Dovyrenite | Ca6Zr(Si2O7)2(OH)4 |
| 9.BE.25 | Lamprophyllite | (Na,Mn2+)3(Sr,Na)2(Ti,Fe3+)3(Si2O7)2O2(OH,O,F)2 |
| 9.BE.25 | Seidozerite | Na4MnZr2Ti(Si2O7)2O2F2 |
| 9.BE.25 | Nabalamprophyllite | (BaNa)Ti2Na3Ti(Si2O7)2O2(OH)2 |
| 9.BE.25 | Schüllerite | Ba2Na(Mn,Ca)(Fe3+,Mg,Fe2+)2Ti2(Si2O7)2(O,F)4 |
| 9.BE.25 | Ericssonite | BaMn2+2Fe3+(Si2O7)O(OH) |
| 9.BE.25 | Grenmarite | Na4MnZr3(Si2O7)2O2F2 |
| 9.BE.25 | Kazanskyite | BaNa3Ti2Nb(Si2O7)2O2(OH)2(H2O)4 |
| 9.BE.25 | Saamite | Ba◻Na3Ti2Nb(Si2O7)2O2(OH)F(H2O)2 |
| 9.BE.25 | Emmerichite | Ba2Na(Na,Fe2+)2(Fe3+,Mg)Ti2(Si2O7)2O2F2 |
| 9.BE.25 | Barytolamprophyllite | (Ba,Na)2(Na,Ti,Fe3+)4Ti2(Si2O7)2O(OH,F) |
| 9.BE.25 | 'Ericssonite-2O' | BaMn2+2Fe3+(Si2O7)O(OH) |
| 9.BE.25 | Fluorbarytolamprophyllite | (Ba,Sr)2[(Na,Fe2+)3(Ti,Mg)F2][Ti2(Si2O7)2O2] |
| 9.BE.25 | Fluorlamprophyllite | Na3(SrNa)Ti3(Si2O7)2O2F2 |
| 9.BE.25 | Lileyite | Ba2(Na,Fe,Ca)3MgTi2(Si2O7)2O2F2 |
| 9.BE.27 | Kolskyite | CaNa2Ti4(Si2O7)2O4(H2O)7 |
| 9.BE.27 | Vigrishinite | NaZnTi4(Si2O7)2O3(OH)(H2O)4 |
| 9.BE.27 | Selivanovaite | NaFe3+Ti4(Si2O7)2O4(H2O)4 |
| 9.BE.27 | Murmanite | Na2Ti2(Si2O7)O2 · 2H2O |
| 9.BE.30 | Epistolite | (Na◻)Nb2Na3Ti(Si2O7)2O2(OH)2(H2O)4 |
| 9.BE.32 | Lomonosovite | Na5Ti2(Si2O7)(PO4)O2 |
| 9.BE.35 | Vuonnemite | Na11Ti4+Nb2(Si2O7)2(PO4)2O3(F,OH) |
| 9.BE.37 | Sobolevite | Na13Ca2Mn2Ti3(Si2O7)2(PO4)4O3F3 |
| 9.BE.40 | Ferroinnelite | Ba4Ti2Na(NaFe2+)Ti(Si2O7)2[(SO4)(PO4)]O2[O(OH)] |
| 9.BE.40 | Phosphoinnelite | Na3Ba4Ti3(Si2O7)2(PO4,SO4)2O2F |
| 9.BE.40 | Innelite | Ba4Ti2Na(NaMn2+)Ti(Si2O7)2[(SO4)(PO4)]O2[O(OH)] |
| 9.BE.42 | Yoshimuraite | Ba2Mn2Ti(Si2O7)(PO4)O(OH) |
| 9.BE.42 | Horiite | Ba2Mn2Mn4Ti2(Si2O7)2(PO4)2O2(OH)2 |
| 9.BE.45 | Quadruphite | Na6Na2(CaNa)2Na2Ti2Na2Ti2(Si2O7)2(PO4)4O4F2 |
| 9.BE.47 | Polyphite | Na5(Na4Ca2)Ti2(Si2O7)(PO4)3O2F2 |
| 9.BE.50 | Shkatulkalite | Na2Nb2Na3Ti(Si2O7)2O2(FO)(H2O)4(H2O)3 |
| 9.BE.50 | Bornemanite | Na6BaTi2Nb(Si2O7)2(PO4)O2(OH)F |
| 9.BE.55 | Hejtmanite | Ba2Mn2+4Ti2(Si2O7)2O2(OH)2F2 |
| 9.BE.55 | Bykovaite | (Ba,Na,K)2(Na,Ti,Mn)4(Ti,Nb)2(Si2O7)2O2(H2O,F,OH)2 · 3.5H2O |
| 9.BE.55 | Nechelyustovite | (Ba,Sr,K)2(Na,Ti,Mn)4(Ti,Nb)2(Si2O7)2O2(O,H2O,F)2 · 4.5H2O |
| 9.BE.55 | Bafertisite | Ba2Fe2+4Ti2(Si2O7)2O2(OH)2F2 |
| 9.BE.60 | Delindeite | (Na,K)2(Ba,Ca)2(Ti,Fe,Al)3(Si2O7)2O2(OH)2 · 2H2O |
| 9.BE.62 | 'Orthochevkinite' | (Ce,La,Ca,Na,Th)4(Fe2+,Mg)2(Ti,Fe3+)3Si4O22 |
| 9.BE.62 va | 'Strontium Perrierite' | (Ce,Sr,La,Ca)4Fe2+(Ti,Zr,Fe)2Ti2(Si2O7)2O8 |
| 9.BE.62 | 'Chevkinite-(Nd)' | (Nd,REE)4(Fe2+,Mg)(Fe2+,Ti,Fe3+)2(Ti,Fe3+)2(Si2O7)2O8 ? |
| 9.BE.62 | 'Perrierite-(Nd)' | Nd4MgFe3+2Ti2(Si2O7)2O8 ? |
| 9.BE.65 | Bussenite | Na2Ba2Fe2+Ti(Si2O7)(CO3)(OH)3F |
| 9.BE.67 | Jinshajiangite | BaNaFe2+4Ti2(Si2O7)2O2(OH)2F |
| 9.BE.67 | Perraultite | BaNaMn2+4Ti2(Si2O7)2O2(OH)2F |
| 9.BE.70 | Dingdaohengite-(Ce) | (Ce,La)4Fe2+(Ti,Fe2+,Mg,Fe3+)2Ti2(Si2O7)2O8 |
| 9.BE.70 | Perrierite-(Ce) | Ce4MgFe3+2Ti2(Si2O7)2O8 |
| 9.BE.70 | Karnasurtite-(Ce) | (Ce,La,Th)(Ti,Nb)(Al,Fe)(Si2O7)(OH)4 · 3H2O |
| 9.BE.70 | Maoniupingite-(Ce) | (Ce,Ca)4(Fe3+,Ti,Fe2+,◻)(Ti,Fe3+,Fe2+,Nb)4(Si2O7)2O8 |
| 9.BE.70 | Matsubaraite | Sr4Ti5(Si2O7)2O8 |
| 9.BE.70 | Rengeite | Sr4ZrTi4(Si2O7)2O8 |
| 9.BE.70 | Polyakovite-(Ce) | (Ce,Ca)4(Mg,Fe2+)(Cr3+,Fe3+)2(Ti,Nb)2(Si2O7)2O8 |
| 9.BE.70 | Hezuolinite | (Sr,REE)4Zr(Ti,Fe3+)4(Si2O7)2O8 |
| 9.BE.70 | 'UM2008-53-SiO:SrTiZr' | Sr4ZrTi4(Si2O7)2O8 |
| 9.BE.70 | Chevkinite-(Ce) | Ce4(Ti,Fe2+,Fe3+)5O8(Si2O7)2 |
| 9.BE.70 | Perrierite-(La) | (La,Ce,Ca)4(Fe2+,Mn)(Ti,Fe3+,Al)4[(Si2O7)O4]2 |
| 9.BE.70 | Strontiochevkinite | (Sr,La,Ce,Ca)4Fe2+(Ti,Zr)2Ti2(Si2O7)2O8 |
| 9.BE.72 | Fersmanite | Ca4(Na,Ca)4(Ti,Nb)4(Si2O7)2O8F3 |
| 9.BE.75 | Belkovite | Ba3(Nb,Ti)6(Si2O7)2O12 |
| 9.BE.77 | Nasonite | Pb6Ca4(Si2O7)3Cl2 |
| 9.BE.80 | Melanotekite | Pb2Fe3+2(Si2O7)O2 |
| 9.BE.80 | Kentrolite | Pb2Mn3+2(Si2O7)O2 |
| 9.BE.82 | Alexkuznetsovite-(La) | La2Mn(CO3)(Si2O7) |
| 9.BE.82 | Tilleyite | Ca5(Si2O7)(CO3)2 |
| 9.BE.85 | Killalaite | Ca6.4(H0.6Si2O7)2(OH)2 |
| 9.BE.87 | Stavelotite-(La) | (La,Nd,Ca)3Mn2+3Cu(Mn3+,Fe3+,Mn4+)26(Si2O7)6O30 |
| 9.BE.90 | Magnesiorowlandite-(Y) | Y4(Mg,Fe)(Si2O7)2F2 |
| 9.BE.90 | Biraite-(Ce) | Ce2Fe2+(Si2O7)(CO3) |
| 9.BE.92 | Cervandonite-(Ce) | (Ce,Nd,La)(Fe3+,Fe2+,Ti,Al)3O2(Si2O7)(As3+O3)(OH) |
| 9.BE.92 | Chirvinskyite | (Na,Ca)13(Fe,Mn,◻)2(Ti,Zr)5(Si2O7)4(OH,O)12 · 2H2O |
| 9.BE.95 | Rusinovite | Ca10(Si2O7)3Cl2 |
| 9.BE.95 | Batisivite | BaV3+8Ti6(Si2O7)O22 |
| 9.BE.97 | Schlüterite-(Y) | (Y,REE)2AlSi2O7(OH)2F |
Other Information
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 Låvenite
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References for Låvenite
Reference List:
Brögger, W. C. (1878) 1. Das Krystallsystem des Mosandrit, in XIX. Untersuchungen norwegischer Mineralien. Zeitschrift für Kristallographie - Crystalline Materials, 2 (1). 275-277erronously described as mosandrite
Brögger, W. C. (1885) Forelöbig meddelelse om to nye norske mineraler, Låvenit og Cappelenit. Geologiska Föreningen i Stockholm Förhandlingar, 7 (10) 598-600 doi:10.1080/11035898509443558
Kutukova, E.I. (1940) Titanolavenite of the Lovozero tundras. Trudy Ign. Akad. Nauk SSSR: 3l: 23-29.
Mellini, M. (1981) Refinement of the crystal structure of låvenite. TMPM Tschermaks Mineralogische und Petrographische Mitteilungen, 28 (2) Springer Science and Business Media LLC. 99-112 doi:10.1007/bf01081548
Perchiazzi, N., McDonald, A. M., Gault, R. A., Johnsen, O., Merlino, S. (2000) The crystal structure of normandite and its crystal-chemical relationships with låvenite. The Canadian Mineralogist, 38 (3). 641-648 doi:10.2113/gscanmin.38.3.641
Friis, Henrik, Balic-Žunić, Tonči (2010) Minerals of the låvenite group from south Greenland and Norway. Norsk Bergverksmuseum Skrift, 43. 35-39 includes description of a låvenite-like mineral, apparently a polytype of burpalite
Localities for Låvenite
Showing 101 localities.
Locality List
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(TL) - Type Locality for a valid mineral species.
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All localities listed without proper references should be considered as questionable.
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Água de Pau Volcano, São Miguel, Azores, Portugal