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Désorite

A valid IMA mineral species
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About DésoriteHide

03058780017271954173043.jpg
Joy Désor
Formula:
Pb2(Fe3+6Zn)O2(PO4)4(OH)8
Colour:
brownish red
Lustre:
Adamantine
Hardness:
3
Specific Gravity:
4.633 (Calculated)
Crystal System:
Triclinic
Name:
Honours Joy Désor (b. 1990), for his tireless analytical work on mineral unknowns, which has led to the discovery and description of the new minerals ammoniotinsleyite, bojarite, oberwolfachite, oldsite-(K), theuerdankite and hanauerite. Joy did the initial work that suggested that the new mineral described herein could be new. At Joy’s suggestion, the name désorite also honours his noteworthy ancestor Pierre Jean Édouard Désor (13 February 1811, Friedrichsdorf, Grand Duchy of Hesse – 23 February 1882 Nice), a Swiss geologist and professor at Neuchâtel Academy (now the University of Neuchâtel). He was a colleague of Louis Agassiz, among others. His studies on paleontology and glacial phenomena in Europe and North America are of particular note. He was a collaborator on the geological survey of the Lake Superior mineral district in the USA.

05396840017271954174085.jpg
Pierre Jean Édouard Désor
Isostructural with:
Unique combination of elements (at the upload time).


Name EncodingHide

ASCII-7:
Desorite

Unique IdentifiersHide

Mindat ID:
470997
Long-form identifier:
mindat:1:1:470997:4

Similar NamesHide

IMA Classification of DésoriteHide

Classification of DésoriteHide

8.BK.25

8 : PHOSPHATES, ARSENATES, VANADATES
B : Phosphates, etc., with additional anions, without H2O
K : With medium-sized and large cations, (OH, etc.):RO4 = 2:1, 2.5:1

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

Physical Properties of DésoriteHide

Adamantine
Transparency:
Transparent
Colour:
Brownish red
Streak:
Orange
Hardness:
Tenacity:
Brittle
Cleavage:
Perfect
two cleavages: {021} perfect and {001} good.
Fracture:
Splintery
Comment:
splintery and curved fracture
Density:
4.633 g/cm3 (Calculated)

Optical Data of DésoriteHide

Type:
Biaxial (+)
RI values:
nα = 2.00(1) nβ = 2.02 nγ = 2.10
2V:
Measured: 54° (2)
Max. Birefringence:
δ = 0.100
Based on recorded range of RI values above.

Interference Colours:
The colours simulate birefringence patterns seen in thin section under crossed polars. They do not take into account mineral colouration or opacity.

Michel-Levy Bar The default colours simulate the birefringence range for a 30 µm thin-section thickness. Adjust the slider to simulate a different thickness.

Grain Simulation You can rotate the grain simulation to show how this range might look as you rotated a sample under crossed polars. Each grain retains its interference colour (retardation) while its brightness falls to black at extinction and reaches a maximum between extinction positions.

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
Interference Figure:
This shows the idealized biaxial acute bisectrix (Bxa) interference figure - the conoscopic view for a grain cut perpendicular to the acute bisectrix, using this mineral's 2V. The two small white dots mark the melatopes - the points where the two optic axes emerge - and are shown only when they fall within the field of view. The coloured bands are isochromatics, and the dark bands are isogyres.

Rotate the stage: at 0°/90° the isogyres form a cross through the melatopes; at 45° they pull apart into curved hyperbolas. That splitting on rotation - absent in a uniaxial figure - is the standard diagnostic test for telling biaxial minerals from uniaxial ones. If 2V is large, the melatopes may fall outside the field of view, as they often do at the microscope too.
Pleochroism:
Strong
Comments:
The mineral is pleochroic: X yellow brown, Y red brown, Z red brown; X < Y ≈ Z.
Comments:
β = 2.02(calc) and γ = 2.10(calc)

Chemistry of DésoriteHide

Mindat Formula:
Pb2(Fe3+6Zn)O2(PO4)4(OH)8
Element Weights:
Element% weight
O30.524 %
Pb30.408 %
Fe24.587 %
P9.091 %
Zn4.798 %
H0.592 %

Calculated from ideal end-member formula.
O
Pb
Fe
P
Zn
H

Crystallography of DésoriteHide

Crystal System:
Triclinic
Class (H-M):
1 - Pinacoidal
Space Group:
P1
Cell Parameters:
a = 5.4389(7) Å, b = 9.324(1) Å, c = 10.093(1) Å
α = 109.024(8)°, β = 90.521(6)°, γ = 97.588(7)°
Ratio:
a:b:c = 0.583 : 1 : 1.082
Unit Cell V:
478.90 ų (Calculated from Unit Cell)
Z:
1
Morphology:
Irregular blades up to about 0.25 mm long, occurring in subparallel and radial aggregates.
Twinning:
none

X-Ray Powder DiffractionHide

Type Occurrence of DésoriteHide

General Appearance of Type Material:
Irregular blades up to about 0.25 mm long, occurring in subparallel and radial aggregates.
Place of Conservation of Type Material:
In the collections of Natural History Museum of Los Angeles County, 900 Exposition Boulevard, Los Angeles, CA 90007, USA, catalogue number 76300
Geological Setting of Type Material:
secondary, oxidation-zone mineral assemblage in vugs in a goethite-quartz gossan
Associated Minerals at Type Locality:

Other Language Names for DésoriteHide

Dutch:Désoriet
German:Désorit

Related Minerals - Strunz-mindat GroupingHide

8.BK.05BrazilianiteNaAl3(PO4)2(OH)4Mon. 2/m : P21/c
8.BK.10NeustädteliteBi2Fe3+(Fe3+,Co)(AsO4)2(O,OH)4Tric. 1 : P1
8.BK.10CobaltneustädteliteBi2Fe3+(Co,Fe3+)(AsO4)2(O,OH)4Tric. 1 : P1
8.BK.10MedenbachiteBi2Fe3+Cu2+(AsO4)2O(OH)3Tric. 1 : P1
8.BK.15CuretoniteBa(Al,Ti)(PO4)(OH,O)FMon. 2/m : P21/c
8.BK.20HeyitePb5Fe2+2(VO4)2O4Mon. 2/m : P21/m
8.BK.25JamesitePb2Zn(Fe2+,Zn)2Fe3+4(AsO4)4(OH)10Tric. 1 : P1
8.BK.25LulzaciteSr2Fe2+(Fe2+,Mg)2Al4(PO4)4(OH)10Tric. 1 : P1
8.BK.30NishanbaeviteKAl2O(AsO4)(SO4)Orth. mmm(2/m2/m2/m) : Pbcm
8.BK.35ZircarsiteNa18Cu12ZrO8(AsO4)8Cl6Iso. m3m(4/m32/m) : Pm3m
8.BK.35ArsmiranditeNa18Cu12Fe3+O8(AsO4)8Cl5Mon. 2/m : B2/m
8.BK.35LebedeviteK4Na14Cu14O8(AsO4)8Cl6Tet. 4/mmm(4/m2/m2/m) : I4/mmm
8.BK.35Lehmannite Na18Cu12TiO8(AsO4)8FCl5Mon. 2/m : B2/m

Fluorescence of DésoriteHide

nonfluorescent in both long- and short-wave ultraviolet illumination

Other InformationHide

Notes:
The mineral is insoluble in room-temperature concentrated HCl.
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 DésoriteHide

References for DésoriteHide

Localities for DésoriteHide

Showing 1 localities.

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.
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Locality ListHide

- This locality has map coordinates listed. - This locality has estimated coordinates. ⓘ - 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.
Germany (TL)
 
  • Rhineland-Palatinate
    • Westerwaldkreis
      • Wirges
        • Dernbach
Bosi et al. (2024) +1 other reference
 
and/or  
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