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Tuliokite

A valid IMA mineral species
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Unique Identifiers
Approval year:
1988

Classification of Tuliokite

5 : CARBONATES (NITRATES)
C : Carbonates without additional anions, with H2O
B : With large cations (alkali and alkali-earth carbonates)

Dana 8th ed.:
15.4.6.1

15 : HYDRATED NORMAL CARBONATES
4 : AmBn(XO3)p·xH2O, with (m+n):p < 1:1
Hey's CIM Ref.:
11.9.6

11 : Carbonates
9 : Carbonates of Pb, Zr and Th

Mineral Symbols
Transparency:
Transparent, Translucent
Colour:
Colourless, white
Comment:
May contain finely dispered inclusions of iron-bearing sulphides or solid organics which makes the color dark-grey to black.
Streak:
White
Tenacity:
Brittle
Cleavage:
None Observed
Fracture:
Conchoidal
Density:
3.15(1) g/cm3 (Measured)    3.25 g/cm3 (Calculated)

Optical Data of Tuliokite
Surface Relief:
Moderate

Chemistry of Tuliokite
Common Impurities:
ORG

Chemical AnalysisYakovenchuk, V. N., Ivanyuk, G. Yu., Pakhomovsky, Ya. A., Men’shikov, Yu. P., Konopleva, N. G., Korchak, Yu. A. (2008) Pyroxenes of the Khibiny alkaline pluton, Kola Peninsula.Geology of Ore Deposits, 50 (8) 732-745doi:10.1134/s1075701508080096Ideal composition

Crystallography of Tuliokite
General Appearance of Type Material:
prismatic to rhombohedral crystals, to 4 mm.
Place of Conservation of Type Material:
Geology Museum, Kola Branch, Academy of Sciences, Apatity, 5947; Mining Institute, St. Petersburg, 2024/1; A.E. Fersman Mineralogical Museum, Academy of Sciences, Moscow, Russia, r430/2.
Geological Setting of Type Material:
Hydrothermal vein within urtite
Associated Minerals at Type Locality:

Synonyms of Tuliokite

Other Language Names for Tuliokite

Common AssociatesMon. 2/m :B2/b5.CB.05ThermonatriteNa2CO3 · H2OOrth.mmm(2/m2/m2/m) :Pmmm5.CB.10NatronNa2CO3 · 10H2OMon. 2/m :P2/m5.CB.15TronaNa3H(CO3)2 · 2H2OMon. 2/m5.CB.20MonohydrocalciteCaCO3 · H2OTrig. 3 :P315.CB.25IkaiteCaCO3 · 6H2OMon. 2/m :B2/b5.CB.30PirssoniteNa2Ca(CO3)2 · 2H2OOrth.mm2 :Fdd25.CB.35GaylussiteNa2Ca(CO3)2 · 5H2OMon. 2/m :B2/b5.CB.40ChalconatroniteNa2Cu(CO3)2 · 3H2OMon. 2/m5.CB.45BaylissiteK2Mg(CO3)2 · 4H2OMon. 2/m :P21/m

Radioactivityshield). This calculation provides a 'worst-case' or 'maximum risk' estimate because it assumes the sample is a point source and entirely neglects any self-shielding where radiation is absorbed within the mineral itself, meaning actual doses will typically be lower. The resulting dose rate (D) is expressed in microsieverts per hour (μSv/h).

D = ((AU × ΓU) + (ATh × ΓTh) + (AK × ΓK)) / r2 × μshield

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  • References for TuliokiteKirovskii apatite mine (TL)Yakovenchuk et al. (1990)+1 other reference
     
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