Almeidaite (original) (raw)

A valid IMA mineral species

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About AlmeidaiteHide

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Formula:

PbZn2(Mn,Y)(Ti,Fe3+)18O37(OH,O)

Name:

Named in 2013 by Luiz Albert Diaz Menezes Filho, L.A.D., N.V. Chukanov, Ramiza K. Rastsvetaeva, S.M. Aksenov, Igor Viktorovich Pekov, M.L.S.C. Chaves, R. Scholz, Daniel Atencio, P.R.G. Brandão, A.W. Romano, L.C.A. de Oliveira, J.D. Ardisson, K. Krambrock, R.L. Moreira, F.S. Guimarães, A.C. Persiano, and R. P. Richards in honor of Prof. Fernando Flávio Marques de Almeida [February 18, 1916 Rio de Janeiro, Brazil - August 2, 2013 São Paulo, Brazil]. Flávio Marques de Almeida is considered to be one of the most important Brazilian geologists. He was professor of geology at Institute for Technological Research, São Paulo about 1938-1939 until 1974. He became professor at the Institute of Geosciences, University of São Paulo, He was one of the founders of the Brazilian Society of Geology and the first chief editor of the Journal of Geology. His honors include: Vice-President of Géologique Société de France (1971); Medal Jose Bonifacio - Society Brazilian Geology (1964), Grand Cross of the National Order of Scientific Merit (1995), Doctor Honoris Causa State University of Campinas (1991), Medal of Merit Council Federal Engineering and Architecture (1995).

The Zn analogue of senaite and Pb analogue of landauite. ZnMn-analogue of cleusonite. PbZn-analogue of crichtonite. Chemically somewhat similar to nežilovite.

Almeidaite is a member of the crichtonite group with Pb dominant in the A site (with 12-fold coordination, located in the cubic layer, _M_0) and Zn dominant in the T site (with 4-fold, i.e., tetrahedral coordination). The anionic cp (close packed) framework has 9 layers along c in the chhchh sequence.

Unique IdentifiersHide

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Long-form identifier:

mindat:1:1:43884:7

1c382261-3629-400e-b26c-ba733cc7dbe2

IMA Classification of AlmeidaiteHide

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IMA Formula:

PbZn2(Mn,Y)(Ti,Fe3+)18O36(OH,O)2

Type description reference:

Menezes Filho, Luiz A. D., Chukanov, Nikita V., Rastsvetaeva, Ramiza K., Aksenov, Sergey M., Pekov, Igor V., Chaves, Mário L. S. C., Richards, R. Peter, Atencio, Daniel, Brandão, Paulo R. G., Scholz, Ricardo, Krambrock, Klaus, Moreira, Roberto L., Guimarães, Frederico S., Romano, Antônio W., Persiano, Aba C., de Oliveira, Luiz C. A., Ardisson, José D. (2015) Almeidaite, Pb(Mn,Y)Zn2(Ti,Fe3+)18O36(O,OH)2, a new crichtonite-group mineral, from Novo Horizonte, Bahia, Brazil. Mineralogical Magazine, 79 (2) 269-283 doi:10.1180/minmag.2015.079.2.06

Classification of AlmeidaiteHide

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4.00.

4 : OXIDES (Hydroxides, V[5,6] vanadates, arsenites, antimonites, bismuthites, sulfites, selenites, tellurites, iodates)
0 :
0 :

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
Amd 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 AlmeidaiteHide

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Density:

4.68(5) g/cm3 (Measured) 4.616 g/cm3 (Calculated)

Optical Data of AlmeidaiteHide

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Reflectivity:

Wavelength R1 R2
400nm 12.84% 15.45%
420nm 12.79% 15.39%
440nm 12.77% 15.36%
460nm 12.79% 15.35%
470nm 12.78% 15.39%
480nm 12.80% 15.39%
500nm 12.77% 15.34%
520nm 12.83% 15.41%
540nm 12.84% 15.41%
546nm 12.86% 15.43%
560nm 12.89% 15.48%
580nm 12.85% 15.42%
589nm 12.91% 15.55%
600nm 12.96% 15.63%
620nm 12.99% 15.67%
640nm 13.02% 15.73%
650nm 13.04% 15.75%
660nm 13.09% 15.81%
680nm 13.11% 15.86%
700nm 13.16% 15.94%

Reflectance graph
Graph shows reflectance levels at different wavelengths (in nm). Top of box is 100%. Peak reflectance is 15.94%.
R1 shown in black, R2 shown in red

Chemistry of AlmeidaiteHide

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Mindat Formula:

PbZn2(Mn,Y)(Ti,Fe3+)18O37(OH,O)

Common Impurities:

Fe,Y,Sr,(Ca,La)

Crystallography of AlmeidaiteHide

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Class (H-M):

3 - Rhombohedral

Cell Parameters:

a = 10.4359(2) Å, c = 21.0471(4) Å

Morphology:

Platy crystals flattened on [0001],dominated by the basal pinacoid {0001}, which is bounded by various, mostly steep, rhombohedra and the hexagonal prism {1120}.

Twinning:

Multiply twinned, with non-planar contact surfaces that are approximately parallel to the c axis.

Crystal StructureHide

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ID Species Reference Link Year Locality Pressure (GPa) Temp (K)
0020510 Almeidaite Kastsvetaeva R K, Aksenov S M, Chukanov N V, Menezes L A D (2014) Crystal structure of almeidaite, a new mineral of the crichtonite group Doklady Chemistry 455 53-57 2014 Novo Horizonte, Bahia, Brazil 0 293

CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

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Powder Diffraction Data:

d-spacing Intensity
3.436 Å (48)
3.074 Å (50)
3.023 Å (50)
2.907 Å (100)
2.781 Å (44)
2.492 Å (55)
2.157 Å (55)
1.615 Å (50)

Comments:

From Type Description.

Geological EnvironmentHide

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Type Occurrence of AlmeidaiteHide

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General Appearance of Type Material:

Isolated, black platy crystals up to 30 × 30 × 6 mm in size.

Place of Conservation of Type Material:

Type material is deposited in the collections of the collections of the Museu de Geociencias, Instituto de Geociencias, Universidade de Saõ Paulo, Saõ Paulo, Brazil, registration number DR744

Associated Minerals at Type Locality:

Reference:

Menezes Filho, L.A.D., Chukanov, N.V., Rastsvetaeva, R.K., Aksenov, S.M., Pekov, I.V., Chaves, M.L.S.C., Richards, R.P., Atencio, D., Brandão, P.R.G., Scholz, R., Krambrock, K., Moreira, R.L., Guimarães, F.S., Romano, A.W., Persiano, A.C., de Oliveira, L.C.A., Ardisson, J.D. (2015) Almeidaite, Pb(Mn,Y)Zn2(Ti,Fe3+)18O36(O,OH)2, a new crichtonite-group mineral, from Novo Horizonte, Bahia, Brazil. Mineralogical Magazine: 79: 269–283.

Synonyms of AlmeidaiteHide

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Relationship of Almeidaite to other SpeciesHide

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Other Members of this group:

Botuobinskite SrFe2+Mg2(Cr3+6Ti4+12)[O36(OH)2] Trig. 3 : _R_3
Cleusonite (Pb,Sr)(U4+,U6+)(Fe2+,Zn)2(Ti,Fe2+,Fe3+)18(O,OH)38 Trig. 3 : _R_3
Crichtonite Sr(Mn,Y,U)Fe2(Ti,Fe,Cr,V)18(O,OH)38 Trig. 3 : _R_3
Davidite-(Ce) Ce(Y,U)Fe2(Ti,Fe,Cr,V)18(O,OH,F)38 Trig. 3 : _R_3
Davidite-(La) La(Y,U)Fe2(Ti,Fe,Cr,V)18(O,OH,F)38 Trig. 3 : _R_3
Davidite-(Y) (La,Ce,Na,Ca,Pb)(Y,Fe2+,◻)(Fe2+,Mn2+)2(Ti,Fe3+,Nb,Zr)18O38 (hypothetical) Trig.
Dessauite-(Y) (Sr,Pb)(Y,U)(Ti,Fe3+)20O38 Trig. 3 : _R_3
Gramaccioliite-(Y) (Pb,Sr)(Y,Mn)Fe3+2(Ti,Fe3+)18O38 Trig. 3 : _R_3
Haitaite-(La) LaU4+Fe3+2(Ti13Fe2+4Fe3+)O38 Trig. 3 : _R_3
Landauite NaMnZn2(Ti,Fe)6Ti12O38 Trig. 3 : _R_3
Lindsleyite (Ba,Sr)(Zr,Ca)(Fe,Mg)2(Ti,Cr,Fe)18O38 Trig.
Loveringite (Ca,Ce,La)(Zr,Fe)(Mg,Fe)2(Ti,Fe,Cr,Al)18O38 Trig. 3 : _R_3
Mapiquiroite (Sr,Pb)(U,Y)Fe2(Ti,Fe3+,Cr3+)18O38 Trig. 3 : _R_3
Mathiasite (Mg,Cr,Fe,Ca,K)2(Ti,Zr,Cr,Fe)5O12 Trig. 3 : _R_3
Mianningite (◻,Pb,Ce,Na)(U4+,Mn,U6+)Fe3+2 (Ti,Fe3+)18O38 Trig. 3 : _R_3
Mirnyite SrZr4+Mg2(Cr3+6Ti4+12)O38 Trig. 3 : _R_3
Paseroite PbMn2+(Mn2+,Fe3+)2(V5+,Ti,◻)18O38 Trig. 3 : _R_3
Saranovskite SrCaFe2+2(Cr4Ti2)Ti12O38 Trig. 3 : _R_3
Senaite Pb(Mn,Y,U)(Fe,Zn)2(Ti,Fe,Cr,V)18(O,OH)38 Trig. 3 : _R_3
UM1987-03-O:FePbTiU ~(U,Pb)(Ti,Fe3+,Fe2+,Mn)21O38 Trig. 3 : _R_3
UM2003-08-O:AlCaFeREEScTiV (Ca,Ce)Sc(Ti,V,Fe,Al)20O38
UM2006-05-O:CaFeKMnNaREESrTiZr (Sr,Na,K,REE)(Ca,Zr,Mn)(Ti,Fe)18Fe2O38
UM2006-06-O:CaFeKMnNaREESrTiZr (Sr,Na,K,REE)(Zr,Ca,Mn)(Ti,Fe)18Fe2O38
UM2006-07-O:CaFeKMnNaREESrTiZr (Na,Sr,K,REE)(Ca,Zr,Mn)(Ti,Fe)18Fe2O38
UM2006-08-O:CaFeKMnNaREESrTiZr (Na,Sr,K,REE)(Zr,Ca,Mn)(Ti,Fe)18Fe2O38
UM2006-09-O:CaFeMnREESrTiZr (Ce,Sr,REE)(Ca,Mn,Zr)Fe2(Ti,Fe)18O38
Unnamed (HBU UK-4) NaFe2+Zn2(Ti,Fe3+,Nb)6Ti12O38 Trig. 3 : _R_3

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4.00. Goethite α-Fe3+O(OH) Orth. m m m _(_2/_m_2/_m_2/m )
4.00. Microlite Group A2-mTa2X6-wZ-n Iso. m_3_m _(_4/_m_32/m ) : F d_3_m
4.00. Ferrotaaffeite-6N'3S (Be,Zn,Mg)FeAl4O8 Trig. 3_m_ _(_32/m ) : R_3_m
4.00. Pyrochlore Group A2Nb2(O,OH)6Z
4.00. Písekite-(Y) (Y,As,Ca,Fe,U)(Nb,Ti,Ta)O4
4.00. UM2004-19-O:AlCeGdZr (Gd,Ce)4Al2Zr4O17
4.00. UM2004-21-O:CaFeGdZr Ca2Gd4Fe5ZrO15
4.00. UM2004-27-O:GdTi Gd2Ti4O11
4.00. Mapiquiroite (Sr,Pb)(U,Y)Fe2(Ti,Fe3+,Cr3+)18O38 Trig. 3 : _R_3
4.00. Vapnikite Ca2CaUO6 Mon. 2/m

Fluorescence of AlmeidaiteHide

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Non-fluorescent in long-wave or short-wave UV

Other InformationHide

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IR Spectrum:

The main absorption bands of the IR spectrum (cm-1, s = strong, sh = shoulder, w = weak) are: 3340 (O-H stretching vibrations), 1099w, 1041w, 1012w (overtones and Zn-OH bending vibrations), 695sh, 574s, 534s, 485sh (stretching vibrations in octahedra and tetrahedra).

Notes:

Metamict due to trace Th; Mössbauer spectroscopy indicates almost all Fe is trivalent.

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 AlmeidaiteHide

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Reference List:

Menezes Filho, Luiz A. D., Chukanov, Nikita V., Rastsvetaeva, Ramiza K., Aksenov, Sergey M., Pekov, Igor V., Chaves, Mário L. S. C., Richards, R. Peter, Atencio, Daniel, Brandão, Paulo R. G., Scholz, Ricardo, Krambrock, Klaus, Moreira, Roberto L., Guimarães, Frederico S., Romano, Antônio W., Persiano, Aba C., de Oliveira, Luiz C. A., Ardisson, José D. (2015) Almeidaite, Pb(Mn,Y)Zn2(Ti,Fe3+)18O36(O,OH)2, a new crichtonite-group mineral, from Novo Horizonte, Bahia, Brazil. Mineralogical Magazine, 79 (2) 269-283 doi:10.1180/minmag.2015.079.2.06

Localities for AlmeidaiteHide

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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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