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Loranskite-(Y)

A valid IMA mineral species - grandfathered
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About Loranskite-(Y)Hide

Formula:
(Y,Ce,Ca)ZrTaO6 (?)
Colour:
Black; greenish yellow (transmitted light)
Lustre:
Sub-Metallic
Hardness:
5
Specific Gravity:
4.6
Member of:
Name:
Named in honor of Apolloniy Mikhailovich Loranskiy (Аполлоний Михайлович Лоранский) (1847-1917), Inspector of the Mining Institute, St. Petersburg, Russia.
An ill-defined material.
(See http://www.mindat.org/mesg-7-88239.html.)


Unique IdentifiersHide

Mindat ID:
2435
Long-form identifier:
mindat:1:1:2435:4

IMA Classification of Loranskite-(Y)Hide

Approved, 'Grandfathered' (first described prior to 1959)
IMA Formula:
(Y,Ce3+,Ca)(Zr4+,Ta5+)2O6

Classification of Loranskite-(Y)Hide

4.DG.05

4 : OXIDES (Hydroxides, V[5,6] vanadates, arsenites, antimonites, bismuthites, sulfites, selenites, tellurites, iodates)
D : Metal: Oxygen = 1:2 and similar
G : With large (+- medium-sized) cations; chains of edge-sharing octahedra
8.1.5.1

8 : MULTIPLE OXIDES CONTAINING NIOBIUM,TANTALUM OR TITANIUM
1 : ABO4

Mineral SymbolsHide

As of 2021 there are now IMA–CNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.

SymbolSourceReference for Standard
Lrs-YIMA–CNMNCWarr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43

Physical Properties of Loranskite-(Y)Hide

Sub-Metallic
Colour:
Black; greenish yellow (transmitted light)
Streak:
Green-grey
Hardness:
Tenacity:
Brittle
Fracture:
Conchoidal
Density:
4.6 g/cm3 (Measured)    

Optical Data of Loranskite-(Y)Hide

Type:
Isotropic
RI values:
n = 2.06
Surface Relief:
Very High (positive)
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

Chemistry of Loranskite-(Y)Hide

Mindat Formula:
(Y,Ce,Ca)ZrTaO6 (?)

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Near-surface Processes
26 : Hadean detrital minerals
Stage 4b: Highly evolved igneous rocks>3.0
34 : Complex granite pegmatites

Type Occurrence of Loranskite-(Y)Hide

Other Language Names for Loranskite-(Y)Hide

Relationship of Loranskite-(Y) to other SpeciesHide

Member of:
Other Members of Euxenite Group:
Euxenite-(Y)(Y,Ca,Ce,U,Th)(Nb,Ta,Ti)2O6Orth. mmm(2/m2/m2/m) : Pbcn
FersmiteCaNb2O6Orth. mmm(2/m2/m2/m) : Pbcn
Kobeite-(Y)(Y,U)(Ti,Nb)2(O,OH)6 (?)Iso.
Tanteuxenite-(Y)Y(Ta,Nb,Ti)2(O,OH)6Orth. mmm(2/m2/m2/m) : Pbcn
Uranopolycrase(U4+,Y)(Ti,Nb)2O6Orth. mmm(2/m2/m2/m) : Pbcn
Yttrocrasite-(Y)(Y,Th,Ca,U)(Ti,Fe)2(O,OH)6Amor.

Related Minerals - Strunz-mindat GroupingHide

4.DG.05FersmiteCaNb2O6Orth. mmm(2/m2/m2/m) : Pbcn
4.DG.05Uranopolycrase(U4+,Y)(Ti,Nb)2O6Orth. mmm(2/m2/m2/m) : Pbcn
4.DG.05Yttrocrasite-(Y)(Y,Th,Ca,U)(Ti,Fe)2(O,OH)6Amor.
4.DG.05Tanteuxenite-(Y)Y(Ta,Nb,Ti)2(O,OH)6Orth. mmm(2/m2/m2/m) : Pbcn
4.DG.05Euxenite-(Y)(Y,Ca,Ce,U,Th)(Nb,Ta,Ti)2O6Orth. mmm(2/m2/m2/m) : Pbcn
4.DG.05Kobeite-(Y)(Y,U)(Ti,Nb)2(O,OH)6 (?)Iso.
4.DG.10Yttrotantalite-(Y)(Y,U,Fe2+)(Ta,Nb)(O,OH)4Orth.
4.DG.10Clinofergusonite-(Y)YNbO4Mon. 2/m
4.DG.10Clinofergusonite-(Nd)(Nd,Ce)NbO4Mon.
4.DG.10Clinofergusonite-(Ce)CeNbO4Mon. 2/m : B2/m
4.DG.15FoorditeSn2+Nb2O6Mon. 2/m : B2/b
4.DG.15ThoreauliteSn2+Ta2O6Mon. 2/m : B2/b
4.DG.20RaspitePb(WO4)Mon. 2/m : P21/c

Other InformationHide

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 Loranskite-(Y)Hide

References for Loranskite-(Y)Hide

Localities for Loranskite-(Y)Hide

Showing 1 localities.

ⓘ - 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.
Russia (TL)
 
  • Republic of Karelia
    • Pitkyarantsky District
      • Pitkyaranta mining district
Anthony et al. (1997)
 
and/or  
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