Hejtmanite
A valid IMA mineral species
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About Hejtmanite
Formula:
Ba2Mn2+4Ti2(Si2O7)2O2(OH)2F2
Colour:
Brownish to golden yellow
Lustre:
Vitreous
Hardness:
4½
Specific Gravity:
3.97 - 4.06
Crystal System:
Triclinic
Member of:
Name:
Named in honour of Prof. RNDr. Bohuslav Hejtman (12 August 1911 StrannĂĄ u Kamenice nad Lipou - 18 September 2000 Praha), professor of petrology at Charles University in Prague, Czech Republic.
The Mn analogue of bafertisite (redefined as so basing on the Mbolve Hill material).
Previously reported to be monoclinic, which was proved wrong.
Chemistry is somewhat similar to that of perraultite. Compare UM1989-33-SiO:BaHMnTi.
Hejtmanite belongs to a group of titanosilicates built of TS (titanosilicate) and I (intermediate) blocks. In this group the TS block consists of HOH sheets, with H standing for heteropolyhedral sheets (penta- and hexacoordinated), and O for central octahedral (trioctahedral) sheet (Sokolova, 2010).
Hejtmanite is a Group-II TS-block mineral, which indicates that the (Ti+Nb) to (Si2O7) ratio is 2:2. In hejtmanite the O sheet consists of five hexacoordinated MO sites occupied mainly by Mn, surrounded by O or OH. The H sheet has (1) two hexacoordinated MH sites (mainly Ti, surrounded by O or F), and (2) four tetrahedral silicon sites. The I block comprises a layer of [12]Ba atoms, that reside within two AP(1,2) sites. Ba is surrounded by O or F. Four (XO) sites equal to two (XO M) and two (XO A) sites, corresponding to O2(OH)2 (Sokolova et al., 2016).
Previously reported to be monoclinic, which was proved wrong.
Chemistry is somewhat similar to that of perraultite. Compare UM1989-33-SiO:BaHMnTi.
Hejtmanite belongs to a group of titanosilicates built of TS (titanosilicate) and I (intermediate) blocks. In this group the TS block consists of HOH sheets, with H standing for heteropolyhedral sheets (penta- and hexacoordinated), and O for central octahedral (trioctahedral) sheet (Sokolova, 2010).
Hejtmanite is a Group-II TS-block mineral, which indicates that the (Ti+Nb) to (Si2O7) ratio is 2:2. In hejtmanite the O sheet consists of five hexacoordinated MO sites occupied mainly by Mn, surrounded by O or OH. The H sheet has (1) two hexacoordinated MH sites (mainly Ti, surrounded by O or F), and (2) four tetrahedral silicon sites. The I block comprises a layer of [12]Ba atoms, that reside within two AP(1,2) sites. Ba is surrounded by O or F. Four (XO) sites equal to two (XO M) and two (XO A) sites, corresponding to O2(OH)2 (Sokolova et al., 2016).
Unique Identifiers
Mindat ID:
1849
Long-form identifier:
mindat:1:1:1849:0
GUID
(UUID V4):
(UUID V4):
4f0b46fa-35ea-4ea5-8ab5-b6a27a907920
IMA Classification of Hejtmanite
Classification of Hejtmanite
9.BE.55
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
56.2.6b.2
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
14.9.18
14 : Silicates not Containing Aluminum
9 : Silicates of Ti
14 : Silicates not Containing Aluminum
9 : Silicates of Ti
Mineral Symbols
As of 2021 there are now IMAâCNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.
Symbol | Source | Reference |
---|---|---|
Hej | IMAâCNMNC | Warr, L.N. (2021). IMAâCNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43 |
Physical Properties of Hejtmanite
Vitreous
Transparency:
Translucent
Colour:
Brownish to golden yellow
Streak:
Yellow, brown
Hardness:
4½ on Mohs scale
Tenacity:
Brittle
Cleavage:
Perfect
On {100}
On {100}
Parting:
Poor parting on {0kl}
Fracture:
Irregular/Uneven
Density:
3.97 - 4.06 g/cm3 (Measured) 4.29 g/cm3 (Calculated)
Optical Data of Hejtmanite
Type:
Biaxial (-)
RI values:
nα = 1.814 nβ = 1.846 nγ = 1.867
2V:
Measured: 76° to 76.8°, Calculated: 76°
Max Birefringence:
δ = 0.053
Image shows birefringence interference colour range (at 30µm thickness)
and does not take into account mineral colouration.
and does not take into account mineral colouration.
Surface Relief:
Very High
Dispersion:
r > v
Optical Extinction:
X = b; Y ⧠c = 37.9°; Z ⧠a = 15.9°.
Comments:
X = light yellow-green; Y = dark golden yellow; Z = light yellow.
Comments:
Absorption: Y > Z = X.
Chemistry of Hejtmanite
Mindat Formula:
Ba2Mn2+4Ti2(Si2O7)2O2(OH)2F2
Common Impurities:
Fe,Nb,K,(Al,Mg,Na,Cl,Sr,Zr)
Crystallography of Hejtmanite
Crystal System:
Triclinic
Class (H-M):
1 - Pinacoidal
Cell Parameters:
a = 10.716(2) Å, b = 13.795(3) Å, c = 11.778(2) Å
α = 90.07(3)°, β = 112.24(3)°, γ = 90.03(3)°
α = 90.07(3)°, β = 112.24(3)°, γ = 90.03(3)°
Ratio:
a:b:c = 0.777 : 1 : 0.854
Unit Cell V:
1612 Ă
Âł
Comment:
Space group setting is C-1
Crystal Structure
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Data courtesy of the American Mineralogist Crystal Structure Database. Click on an AMCSD ID to view structure
ID | Species | Reference | Link | Year | Locality | Pressure (GPa) | Temp (K) |
---|---|---|---|---|---|---|---|
0020128 | Hejtmanite | Rastsvetaeva R K, Tamazyan R A, Sokolova E V, Belakovskii D I (1991) Crystal structures of two modifications of natural Ba, Mn-titanosilicate Soviet Physics Crystallography 36 186-189 | 1991 | Inyl'chek ridge, southeast Kirgiziya | 0 | 293 | |
0020129 | Hejtmanite | Rastsvetaeva R K, Tamazyan R A, Sokolova E V, Belakovskii D I (1991) Crystal structures of two modifications of natural Ba, Mn-titanosilicate Soviet Physics Crystallography 36 186-189 | 1991 | Inyl'chek ridge, southeast Kirgiziya | 0 | 293 |
CIF Raw Data - click here to close
X-Ray Powder Diffraction
Powder Diffraction Data:
d-spacing | Intensity |
---|---|
2.726 Ă | (100) |
5.472 Ă | (32) |
3.241 Ă | (21) |
3.215 Ă | (21) |
3.455 Ă | (17) |
2.180 Ă | (16) |
3.669 Ă | (14) |
Comments:
Mbolwe Hill, Zambia. Data from the type description.
Geological Environment
Paragenetic Mode(s):
Paragenetic Mode | Earliest Age (Ga) |
---|---|
Near-surface Processes | |
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47) | |
Stage 4b: Highly evolved igneous rocks | >3.0 |
35 : Ultra-alkali and agpaitic igneous rocks |
Type Occurrence of Hejtmanite
General Appearance of Type Material:
Prismatic or platy crystals up to 1 mm long enclosed in manganoan arfvedsonite.
Place of Conservation of Type Material:
Charles University, Praha, Czech Republic (cotype).
National Museum, Praha, Czech Republic (cotype).
National Museum, Praha, Czech Republic (cotype).
Geological Setting of Type Material:
A system of young segregation veins of manganoan arfvedsonite cutting foliated alkali granite and syenite.
Associated Minerals at Type Locality:
Synonyms of Hejtmanite
Other Language Names for Hejtmanite
Relationship of Hejtmanite to other Species
Member of:
Other Members of this group:
Bafertisite | Ba2Fe2+4Ti2(Si2O7)2O2(OH)2F2 | Tric. |
Bobshannonite | Na2KBa(Mn,Na)8(Nb,Ti)4(Si2O7)4O4(OH)4(O,F)2 | Tric. |
Bussenite | Na2Ba2Fe2+Ti(Si2O7)(CO3)(OH)3F | Tric. 1 : P1 |
CĂĄmaraite | Ba3Na(Fe2+,Mn)8Ti4(Si2O7)4O4(OH,F)7 | Tric. 1 |
Jinshajiangite | BaNaFe2+4Ti2(Si2O7)2O2(OH)2F | Tric. 1 : P1 |
Perraultite | BaNaMn2+4Ti2(Si2O7)2O2(OH)2F | Tric. 1 |
Yoshimuraite | Ba2Mn2Ti(Si2O7)(PO4)O(OH) | Tric. 1 : P1 |
Common Associates
Associated Minerals Based on Photo Data:
3 photos of Hejtmanite associated with Rhodonite | CaMn3Mn[Si5O15] |
3 photos of Hejtmanite associated with Quartz | SiO2 |
3 photos of Hejtmanite associated with Aegirine | NaFe3+Si2O6 |
2 photos of Hejtmanite associated with Zektzerite | LiNaZrSi6O15 |
1 photo of Hejtmanite associated with Alabandite | MnS |
1 photo of Hejtmanite associated with Tephroite | Mn2+2SiO4 |
1 photo of Hejtmanite associated with Khristovite-(Ce) | (CaCe)(MgAlMn2+)F[Si2O7][SiO4](OH) |
1 photo of Hejtmanite associated with Fluorite | CaF2 |
Related Minerals - Strunz-mindat Grouping
9.BE. | Paralomonosovite | Na6â»4Ti4(Si2O7)2[PO3OH][PO2(OH)2]O2(OF) |
9.BE. | CĂĄmaraite | Ba3Na(Fe2+,Mn)8Ti4(Si2O7)4O4(OH,F)7 |
9.BE. | ChristofschÀferite-(Ce) | Ce3CaMnTiFe(3+)Ti2(Si2O7)2O8 |
9.BE. | Bobshannonite | Na2KBa(Mn,Na)8(Nb,Ti)4(Si2O7)4O4(OH)4(O,F)2 |
9.BE. | Calciomurmanite | (Na,â»)2Ca(Ti,Mg,Nb)4[Si2O7]2O2(OH,O)2(H2O)4 |
9.BE. | Batievaite-(Y) | Y2Ca2Ti(Si2O7)2(OH)2(H2O)4 |
9.BE. | Delhuyarite-(Ce) | Ce4Mg(Fe3+,W)3â»(Si2O7)2O6(OH)2 |
9.BE.X | Asimowite | Fe2+4O(Si2O7) |
9.BE. | Moxuanxueite | NaCa6Zr(Si2O7)2OF3 |
9.BE. | Alexkuznetsovite-(Ce) | Ce2Mn(CO3)(Si2O7) |
9.BE. | Biraite-(La) | La2Fe2+(CO3)(Si2O7) |
9.BE. | Zinkgruvanite | Ba4Mn2+4Fe3+2(Si2O7)2(SO4)2O2(OH)2 |
9.BE. | Madeiraite | Na2Ca2Fe2Zr2(Si2O7)2O2F2 |
9.BE. | Bortolanite | Ca2(Ca1.5Zr0.5)Na(NaCa)Ti(Si2O7)2(OF)F2 |
9.BE. | Nacareniobsite-(Y) | Na3Ca3YNb(Si2O7)2OF3 |
9.BE. | Pilanesbergite | Na2Ca2Fe2Ti2(Si2O7)2O2F2 |
9.BE. | Alfredcasparite | Sr2TiO(Si2O7) |
9.BE.02 | Wadsleyite | Mg4O(Si2O7) |
9.BE.05 | Hennomartinite | SrMn3+2(Si2O7)(OH)2 · H2O |
9.BE.05 | Lawsonite | CaAl2(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.05 | Cortesognoite | CaV2(Si2O7)(OH)2 · H2O |
9.BE.07 | Ilvaite | CaFe3+Fe2+2(Si2O7)O(OH) |
9.BE.07 | Manganilvaite | CaFe2+Fe3+Mn2+(Si2O7)O(OH) |
9.BE.07 | Amamoorite | CaMn2+2Mn3+(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 | Baghdadite | Ca6Zr2(Si2O7)2O4 |
9.BE.17 | Burpalite | Na2CaZr(Si2O7)F2 |
9.BE.17 | Cuspidine | Ca8(Si2O7)2F4 |
9.BE.17 | Hiortdahlite | Na2Ca4(Ca0.5Zr0.5)Zr(Si2O7)2OF3 |
9.BE.17 | Janhaugite | (Na,Ca)3(Mn2+,Fe2+)3(Ti,Zr,Nb)2(Si2O7)2O2(OH,F)2 |
9.BE.17 | LĂ„venite | Na2Ca2Mn2Zr2(Si2O7)2O2F2 |
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 | Wöhlerite | Na2Ca4ZrNb(Si2O7)2O3F |
9.BE.20 | Mosandrite-(Ce) | (Ca3REE)[(H2O)2Ca0.5â»0.5]Ti(Si2O7)2(OH)2(H2O)2 |
9.BE.20 | Nacareniobsite-(Ce) | Na3Ca3(Ce,REE)Nb(Si2O7)2OF3 |
9.BE.20 | Roumaite | (Ca,Na,REE,â»)7(Nb,Ti)[Si2O7]2OF3 |
9.BE.20 | Rinkite-(Y) | Na2Ca4YTi(Si2O7)2OF3 |
9.BE.22 | Götzenite | NaCa6Ti(Si2O7)2OF3 |
9.BE.22 | Hainite-(Y) | Na2Ca4(Y,REE)Ti(Si2O7)2OF3 |
9.BE.22 | Rosenbuschite | Na6Ca6Zr3Ti(Si2O7)4O2F6 |
9.BE.22 | Kochite | Na3Ca2MnZrTi(Si2O7)2OF3 |
9.BE.22 | Fogoite-(Y) | Na3Ca2Y2Ti(Si2O7)2OF3 |
9.BE.23 | Dovyrenite | Ca6Zr(Si2O7)2(OH)4 |
9.BE.25 | Barytolamprophyllite | (Ba,Na)2(Na,Ti,Fe3+)4Ti2(Si2O7)2O(OH,F) |
9.BE.25 | Ericssonite | BaMn2+2Fe3+(Si2O7)O(OH) |
9.BE.25 | Lamprophyllite | (Na,Mn2+)3(Sr,Na)2(Ti,Fe3+)3(Si2O7)2O2(OH,O,F)2 |
9.BE.25 | Ericssonite-2O | BaMn2+2Fe3+(Si2O7)O(OH) |
9.BE.25 | Seidozerite | Na4MnZr2Ti(Si2O7)2O2F2 |
9.BE.25 | Nabalamprophyllite | (BaNa)Ti2Na3Ti(Si2O7)2O2(OH)2 |
9.BE.25 | Grenmarite | Na4MnZr3(Si2O7)2O2F2 |
9.BE.25 | SchĂŒllerite | Ba2Na(Mn,Ca)(Fe3+,Mg,Fe2+)2Ti2(Si2O7)2(O,F)4 |
9.BE.25 | Kazanskyite | BaNa3Ti2Nb(Si2O7)2O2(OH)2(H2O)4 |
9.BE.25 | Lileyite | Ba2(Na,Fe,Ca)3MgTi2(Si2O7)2O2F2 |
9.BE.25 | Emmerichite | Ba2Na(Na,Fe2+)2(Fe3+,Mg)Ti2(Si2O7)2O2F2 |
9.BE.25 | Saamite | Baâ»Na3Ti2Nb(Si2O7)2O2(OH)F(H2O)2 |
9.BE.25 | Fluorlamprophyllite | Na3(SrNa)Ti3(Si2O7)2O2F2 |
9.BE.25 | Fluorbarytolamprophyllite | (Ba,Sr)2[(Na,Fe2+)3(Ti,Mg)F2][Ti2(Si2O7)2O2] |
9.BE.27 | Murmanite | Na2Ti2(Si2O7)O2 · 2H2O |
9.BE.27 | Vigrishinite | NaZnTi4(Si2O7)2O3(OH)(H2O)4 |
9.BE.27 | Kolskyite | CaNa2Ti4(Si2O7)2O4(H2O)7 |
9.BE.27 | Selivanovaite | NaFe3+Ti4(Si2O7)2O4(H2O)4 |
9.BE.30 | Epistolite | (Naâ»)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 | Innelite | Ba4Ti2Na(NaMn2+)Ti(Si2O7)2[(SO4)(PO4)]O2[O(OH)] |
9.BE.40 | Phosphoinnelite | Na3Ba4Ti3(Si2O7)2(PO4,SO4)2O2F |
9.BE.42 | Yoshimuraite | Ba2Mn2Ti(Si2O7)(PO4)O(OH) |
9.BE.45 | Quadruphite | Na6Na2(CaNa)2Na2Ti2Na2Ti2(Si2O7)2(PO4)4O4F2 |
9.BE.47 | Polyphite | Na5(Na4Ca2)Ti2(Si2O7)(PO4)3O2F2 |
9.BE.50 | Bornemanite | Na6BaTi2Nb(Si2O7)2(PO4)O2(OH)F |
9.BE.50 | Shkatulkalite | Na2Nb2Na3Ti(Si2O7)2O2(FO)(H2O)4(H2O)3 |
9.BE.55 | Bafertisite | Ba2Fe2+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.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 | Karnasurtite-(Ce) | (Ce,La,Th)(Ti,Nb)(Al,Fe)(Si2O7)(OH)4 · 3H2O |
9.BE.70 | Perrierite-(Ce) | Ce4MgFe3+2Ti2(Si2O7)2O8 |
9.BE.70 | Strontiochevkinite | (Sr,La,Ce,Ca)4Fe2+(Ti,Zr)2Ti2(Si2O7)2O8 |
9.BE.70 | Chevkinite-(Ce) | Ce4(Ti,Fe2+,Fe3+)5O8(Si2O7)2 |
9.BE.70 | Polyakovite-(Ce) | (Ce,Ca)4(Mg,Fe2+)(Cr3+,Fe3+)2(Ti,Nb)2(Si2O7)2O8 |
9.BE.70 | Rengeite | Sr4ZrTi4(Si2O7)2O8 |
9.BE.70 | Matsubaraite | Sr4Ti5(Si2O7)2O8 |
9.BE.70 | Dingdaohengite-(Ce) | (Ce,La)4Fe2+(Ti,Fe2+,Mg,Fe2+)2Ti2(Si2O7)2O8 |
9.BE.70 | Maoniupingite-(Ce) | (Ce,Ca)4(Fe3+,Ti,Fe2+,â»)(Ti,Fe3+,Fe2+,Nb)4(Si2O7)2O8 |
9.BE.70 | Perrierite-(La) | (La,Ce,Ca)4(Fe2+,Mn)(Ti,Fe3+,Al)4[(Si2O7)O4]2 |
9.BE.70 | UM2008-53-SiO:SrTiZr | Sr4ZrTi4(Si2O7)2O8 |
9.BE.70 | Hezuolinite | (Sr,REE)4Zr(Ti,Fe3+)4(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 | Kentrolite | Pb2Mn3+2(Si2O7)O2 |
9.BE.80 | Melanotekite | Pb2Fe3+2(Si2O7)O2 |
9.BE.82 | Tilleyite | Ca5(Si2O7)(CO3)2 |
9.BE.82 | Alexkuznetsovite-(La) | La2Mn(CO3)(Si2O7) |
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 | Biraite-(Ce) | Ce2Fe2+(Si2O7)(CO3) |
9.BE.90 | Magnesiorowlandite-(Y) | Y4(Mg,Fe)(Si2O7)2F2 |
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,â»)2(Ti,Zr)5(Si2O7)4(OH,O)12 · 2H2O |
9.BE.95 | Batisivite | BaV3+8Ti6(Si2O7)O22 |
9.BE.95 | Rusinovite | Ca10(Si2O7)3Cl2 |
9.BE.97 | SchlĂŒterite-(Y) | (Y,REE)2AlSi2O7(OH)2F |
Fluorescence of Hejtmanite
Not fluorescent.
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 Hejtmanite
mindat.org URL:
https://www.mindat.org/min-1849.html
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References for Hejtmanite
Reference List:
Sokolova, E., CĂĄmara, F., Hawthorne, F. C., Pautov, L. A. (2016) From structure topology to chemical composition. XX. Titanium silicates: the crystal structure of hejtmanite, Ba2Mn4Ti2(Si2O7)2O2(OH)2F2, a Group-II TS-block mineral. Mineralogical Magazine, 80 (5) 841-853 doi:10.1180/minmag.2016.080.026
Sokolova, E., CĂĄmara, F. (2017) The seidozerite supergroup of TS-block minerals: nomenclature and classification, with change of the following names: rinkite to rinkite-(Ce), mosandrite to mosandrite-(Ce), hainite to hainite-(Y) and innelite-1T to innelite-1A. Mineralogical Magazine, 81 (6) 1457-1484 doi:10.1180/minmag.2017.081.010
Localities for Hejtmanite
Locality List
- This locality has map coordinates listed.
- This locality has estimated coordinates.
â - 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.
All localities listed without proper references should be considered as questionable.
Austria | |
| Kolitsch et al. (2021) |
France | |
| publication date: November 2018 +1 other reference |
Japan | |
| Yamada collection (Crystal World, Japan) |
| Alfredo Petrov collection |
Kyrgyzstan | |
| Pekov (1998) |
Russia | |
| Ganzeev A.A. |
| Lykova |
| Brusnitsyn (2000) |
| Sharygin et al. (2014) |
South Africa | |
| R. Liferovich - L. HorvĂĄth p.c. (2004) |
Tajikistan | |
| Chukanov (2014) |
Ukraine | |
| Victor V. Sharygin analytycal data (2013) |
Zambia (TL) | |
| European Journal of Mineralogy (1992) |
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Dara-i-Pioz Massif, Districts of Republican Subordination, Tajikistan