Carmeltazite (original) (raw)

A valid IMA mineral species

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About CarmeltaziteHide

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Colour:

Dark brown to dark green

Crystal System:

Orthorhombic

Name:

The name carmeltazite derives from the type locality, Mt Carmel (“CARMEL”), and from the dominant metals present in the mineral, i.e., titanium, aluminum and zirconium (“TAZ”).

Has an atomic arrangement similar to that observed in a defective spinel structure.

Found in pockets of trapped melt interstitial to, or included in, corundum crystals.

Represents a relatively small group of minerals in which Zr and Ti are located in separate structural sites.

Awarded 'Mineral of the Year' by the IMA-CNMNC in 2018.

Unique IdentifiersHide

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Long-form identifier:

mindat:1:1:53294:9

aa3295a0-53ae-4945-8a03-4e039d6a4722

IMA Classification of CarmeltaziteHide

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Type description reference:

Griffin, W.L., Gain, S.E.M., Bindi, L., Toledo, V., Cámara, F., Saunders, M., O’Reilly, S.Y. (2018): Carmeltazite, ZrAl2Ti4O11, a New Mineral Trapped in Corundum from Volcanic Rocks of Mt Carmel, Northern Israel. Minerals: 8: 601.

Classification of CarmeltaziteHide

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4.BB.30

4 : OXIDES (Hydroxides, V[5,6] vanadates, arsenites, antimonites, bismuthites, sulfites, selenites, tellurites, iodates)
B : Metal: Oxygen = 3:4 and similar
B : With only medium-sized cations

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
Ctz 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 CarmeltaziteHide

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Colour:

Dark brown to dark green

Optical Data of CarmeltaziteHide

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Bireflectance:

Weak to moderate

Reflectivity:

Wavelength R1 R2
471.1nm 21.8% 22.9%
548.3nm 21.0% 21.6%
586.6nm 19.9% 20.7%
652.3nm 18.5% 19.8%

Reflectance graph
Graph shows reflectance levels at different wavelengths (in nm). Top of box is 100%. Peak reflectance is 22.9%.
R1 shown in black, R2 shown in red

Internal Reflections:

Absent

Comments:

Dark brown to dark green

Chemistry of CarmeltaziteHide

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Mindat Formula:

ZrAl2Ti4O11

Crystallography of CarmeltaziteHide

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Crystal System:

Orthorhombic

Class (H-M):

m m m _(_2/_m_2/_m_2/m ) - Dipyramidal

Cell Parameters:

a = 4.0951(9) Å, b = 5.8123(4) Å, c = 10.0848(7) Å

Ratio:

a:b:c = 0.705 : 1 : 1.735

X-Ray Powder DiffractionHide

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Powder Diffraction Data:

d-spacing Intensity
5.04 Å (65)
4.09 Å (60)
2.961 Å (100)
2.885 Å (40)
2.047 Å (60)

Geological EnvironmentHide

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Type Occurrence of CarmeltaziteHide

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General Appearance of Type Material:

Inclusions in pockets of trapped melt interstitial to, or included in, corundum xenocrysts.

Place of Conservation of Type Material:

Natural History Museum, University of Florence, Italy (3293/I).

Geological Setting of Type Material:

Cretaceous Mt Carmel volcanics of northern Israel.

Associated Minerals at Type Locality:

Reference:

Griffin, W.L., Gain, S.E.M., Bindi, L., Toledo, V., Cámara, F., Saunders, M., O’Reilly, S.Y. (2018) Carmeltazite, ZrAl2Ti4O11, a New Mineral Trapped in Corundum from Volcanic Rocks of Mt Carmel, Northern Israel. Minerals: 8: 601.

Synonyms of CarmeltaziteHide

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Common AssociatesHide

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Associated Minerals Based on Photo Data:

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4.BB. Elgoresyite (Mg5Si2)O9 Mon. 2/m : _B_2/m
4.BB. Chenmingite FeCr2O4 Orth. m m m _(_2/_m_2/_m_2/m ) : P n m a
4.BB. Dellagiustaite V2+Al2O4 Iso. m_3_m _(_4/_m_32/m ) : F d_3_m
4.BB. Thermaerogenite CuAl2O4 Iso. m_3_m _(_4/_m_32/m ) : F d_3_m
4.BB. Chukochenite LiAl5O8 Orth. m m m _(_2/_m_2/_m_2/m ) : I m m a
4.BB. Garpenbergite Mn6◻AsSbO10(OH)2 Orth. m m m _(_2/_m_2/_m_2/m )
4.BB. Magnéliite Ti3+2Ti4+2O7 Tric. 1 : _P_1
4.BB. Jianmuite ZrTi4+Ti3+5Al3O16 Tet. 4 : _I_4
4.BB.05 Chromite Fe2+Cr3+2O4 Iso. m_3_m _(_4/_m_32/m ) : F d_3_m
4.BB.05 Cochromite CoCr2O4 Iso. m_3_m _(_4/_m_32/m ) : F d_3_m
4.BB.05 Coulsonite Fe2+V3+2O4 Iso. m_3_m _(_4/_m_32/m ) : F d_3_m
4.BB.05 Cuprospinel Cu2+Fe3+2O4 Iso. m_3_m _(_4/_m_32/m )
4.BB.05 Filipstadite (Fe3+0.5Sb5+0.5)Mn2O4 Iso.
4.BB.05 Franklinite Zn2+Fe3+2O4 Iso. m_3_m _(_4/_m_32/m ) : F d_3_m
4.BB.05 Gahnite ZnAl2O4 Iso. m_3_m _(_4/_m_32/m ) : F d_3_m
4.BB.05 Galaxite Mn2+Al2O4 Iso. m_3_m _(_4/_m_32/m ) : F d_3_m
4.BB.05 Hercynite Fe2+Al2O4 Iso. m_3_m _(_4/_m_32/m ) : F d_3_m
4.BB.05 Jacobsite Mn2+Fe3+2O4 Iso. m_3_m _(_4/_m_32/m ) : F d_3_m
4.BB.05 Manganochromite Mn2+Cr2O4 Iso. m_3_m _(_4/_m_32/m ) : F d_3_m
4.BB.05 Magnesiocoulsonite MgV2O4 Iso. m_3_m _(_4/_m_32/m )
4.BB.05 Magnesiochromite MgCr2O4 Iso. m_3_m _(_4/_m_32/m ) : F d_3_m
4.BB.05 Magnesioferrite MgFe3+2O4 Iso. m_3_m _(_4/_m_32/m ) : F d_3_m
4.BB.05 Magnetite Fe2+Fe3+2O4 Iso. m_3_m _(_4/_m_32/m ) : F d_3_m
4.BB.05 Nichromite (Ni,Co,Fe)(Cr,Fe,Al)2O4 Iso. m_3_m _(_4/_m_32/m ) : F d_3_m
4.BB.05 Qandilite (Mg,Fe3+)2(Ti,Fe3+,Al)O4 Iso. m_3_m _(_4/_m_32/m ) : F d_3_m
4.BB.05 Spinel MgAl2O4 Iso. m_3_m _(_4/_m_32/m ) : F d_3_m
4.BB.05 Trevorite Ni2+Fe3+2O4 Iso. m_3_m _(_4/_m_32/m ) : F d_3_m
4.BB.05 Ulvöspinel TiFe2+2O4 Iso. m_3_m _(_4/_m_32/m ) : F d_3_m
4.BB.05 Vuorelainenite Mn2+V3+2O4 Iso. m_3_m _(_4/_m_32/m ) : F d_3_m
4.BB.05 Zincochromite ZnCr2O4 Iso. m_3_m _(_4/_m_32/m ) : F d_3_m
4.BB.05 Harmunite CaFe2O4 Orth. m m m _(_2/_m_2/_m_2/m ) : P b c m
4.BB.05 Wernerkrauseite Ca(Fe3+,Mn3+)2Mn4+O6 Orth. m m m _(_2/_m_2/_m_2/m ) : P n m a
4.BB.05 Deltalumite (Al0.67◻0.33)Al2O4 Tet. 42_m_ : _P_4_m_2
4.BB.05 Guite Co2+Co3+2O4 Iso.
4.BB.10 Hausmannite Mn2+Mn3+2O4 Tet. 4/m m m _(_4/_m_2/_m_2/m ) : _I_41/a m d
4.BB.10 Hetaerolite ZnMn2O4 Tet. 4/m m m _(_4/_m_2/_m_2/m ) : _I_41/a m d
4.BB.10 Manganostibite (Mn,Fe)7SbAsO12 Orth. m m m _(_2/_m_2/_m_2/m )
4.BB.15 Maghemite (Fe3+0.67◻0.33)Fe3+2O4 Iso. 432 : _P_4132
4.BB.15 Titanomaghemite (Ti4+0.5◻0.5)Fe3+2O4 Iso. 432 : _P_4332
4.BB.20 Tegengrenite (Mn3+0.5Sb5+0.5)Mg2O4 Trig. 3 : _R_3
4.BB.25 Xieite Fe2+Cr2O4 Orth. m m m _(_2/_m_2/_m_2/m )
4.BB.35 Feiite Fe2+2(Fe2+Ti4+)O5 Orth. m m m _(_2/_m_2/_m_2/m ) : C m c m
4.BB.40 Maohokite MgFe2O4 Orth. m m m _(_2/_m_2/_m_2/m ) : P n m a
4.BB.45 Tschaunerite (Fe2+)(Fe2+Ti4+)O4 Orth. m m m _(_2/_m_2/_m_2/m ) : C m c m

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.

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References for CarmeltaziteHide

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Reference List:

Griffin, W.L., Gain, S.E.M., Bindi, L., Toledo, V., Cámara, F., Saunders, M., O’Reilly, S.Y. (2018): Carmeltazite, ZrAl2Ti4O11, a New Mineral Trapped in Corundum from Volcanic Rocks of Mt Carmel, Northern Israel. Minerals: 8: 601.

Miyawaki, Ritsuro, Hålenius, Ulf, Hatert, Frédéric, Pasero, Marco, Mills, Stuart J. (2019) IMA Commission on New Minerals, Nomenclature and Classification (CNMNC) NEWSLETTER 47. European Journal of Mineralogy, 31 (1) 197-202 doi:10.1127/ejm/2019/0031-2839

Localities for CarmeltaziteHide

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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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