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Thermessaite-(NH4)

A valid IMA mineral species
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About Thermessaite-(NH4)Hide

Formula:
(NH4)2AlF3(SO4)
NH4 may be replaced by minor K.
Colour:
Colourless to white
Lustre:
Vitreous
Specific Gravity:
2.815 (Calculated)
Crystal System:
Orthorhombic
Name:
For being the NH4-analogue of thermessaite.
Isostructural with:
The ammonium analogue of thermessaite.

Also originally found as an anthropogenic compound ('Unnamed (NH4-analogue of Thermessaite)') on a burning coal dump at the Anna mine, Aachen (U. Kolitsch, 2010, unpubl. data on material collected by Frank de Wit; subsequently published in Witzke et al., 2015).

This mineral contains linear infinite chains of repeating (AlF3) units, classifying it as a so-called ino-fluoro-aluminate.

Crystal structure details:

* corner-sharing AlF4O2 octahedra comprising [001] octahedral chains (by sharing two trans fluoride atoms;
* NH4+ ions placed within layers || (100), alternating regularly with (100) layers;
* the latter layers comprise ribbons of the AlF4O2 octahedra and SO4 groups;
* coordination sphere of the ammonium ions bears five oxygen atoms and by four fluorine atoms


Name EncodingHide

Formatted:
thermessaite-(NH4)
HTML:
thermessaite-(NH<sub>4</sub>)
LaTeX:
thermessaite-(NH\$\_4\$)

Unique IdentifiersHide

Mindat ID:
39963
Long-form identifier:
mindat:1:1:39963:6

Similar NamesHide

ThermessaiteA valid IMA mineral speciesK2AlF3(SO4)

IMA Classification of Thermessaite-(NH4)Hide

Approved
Approval year:
2011
First published:
2021

Classification of Thermessaite-(NH4)Hide

3.CG.25

3 : HALIDES
C : Complex halides
G : Aluminofluorides with CO3, SO4, PO4

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
Tms-NH4IMA–CNMNCWarr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43

Physical Properties of Thermessaite-(NH4)Hide

Vitreous
Transparency:
Transparent
Colour:
Colourless to white
Streak:
White
Density:
2.815 g/cm3 (Calculated)

Chemistry of Thermessaite-(NH4)Hide

Mindat Formula:
(NH4)2AlF3(SO4)

NH4 may be replaced by minor K.
Element Weights:
Element% weight
O29.613 %
F26.373 %
S14.837 %
N12.962 %
Al12.485 %
H3.731 %

Calculated from ideal end-member formula.

Crystallography of Thermessaite-(NH4)Hide

Crystal System:
Orthorhombic
Class (H-M):
mmm (2/m 2/m 2/m) - Dipyramidal
Space Group:
Pbcn
Cell Parameters:
a = 11.3005(3) Å, b = 8.6125(3) Å, c = 6.8501(2) Å
Ratio:
a:b:c = 1.312 : 1 : 0.795
Unit Cell V:
666.69 ų (Calculated from Unit Cell)
Morphology:
Acicular.
Comment:
Cell of anthropogenic material: a = 11.286(2), 8.607(2), 6.843(1) A.

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
6.850 Å(74)
5.650 Å(100)
4.844 Å(89)
3.082 Å(47)
3.063 Å(56)
2.782 Å(26)
2.681 Å(28)

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Stage 7: Great Oxidation Event<2.4
45a : [Sulfates, arsenates, selenates, antimonates]
45b : [Other oxidized fumarolic minerals]
Stage 10b: Anthropogenic minerals<10 Ka
54 : Coal and other mine fire minerals (see also #51 and #56)

Type Occurrence of Thermessaite-(NH4)Hide

General Appearance of Type Material:
Micrometer-sized, sharp, prismatic crystals, forming aggregates.
Place of Conservation of Type Material:
Type material is deposited in the collections of the C.L. Garavelli Museum in the Dipartimento di Scienze della Terra e Geoambientali, Università degli Studi di Bari ‘‘Aldo Moro’’, Italy, sample number 15/nm-V28.
Geological Setting of Type Material:
On the surface of pyroclastic breccia.
Associated Minerals at Type Locality:

Synonyms of Thermessaite-(NH4)Hide

Other Language Names for Thermessaite-(NH4)Hide

Related Minerals - Strunz-mindat GroupingHide

3.CG.3.CG.Chukhrovite-(Ca)Ca3Ca1.5Al2(SO4)F13 · 12H2OIso. m3 (2/m 3) : Fd3
3.CG.05StenoniteSr2Al(CO3)F5Mon. 2/m
3.CG.10MeniayloviteCa4[(SO4)(SiF6)(AlF6)]F · 12H2OIso. m3 (2/m 3) : Fd3
3.CG.10Chukhrovite-(Ce)Ca3CeAl2(SO4)F13 · 12H2OIso.
3.CG.10Chukhrovite-(Y)Ca3YAl2(SO4)F13 · 12H2OIso. m3 (2/m 3) : Fd3
3.CG.10Chukhrovite-(Nd)Ca3NdAl2(SO4)F13 · 12H2OIso. m3 (2/m 3) : Fd3
3.CG.15CreediteCa3Al2(SO4)(OH)2F8 · 2H2OMon. 2/m : B2/b
3.CG.20BøggilditeNa2Sr2Al2PO4F9Mon. 2/m : P21/b
3.CG.25ThermessaiteK2AlF3(SO4)Orth. mmm (2/m 2/m 2/m) : Pbcn
3.CG.30KruijeniteCa4Al4(SO4)F2(OH)16 · 2H2OTet. 4/mmm (4/m 2/m 2/m) : P4/nnc

Fluorescence of Thermessaite-(NH4)Hide

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 Thermessaite-(NH4)Hide

References for Thermessaite-(NH4)Hide

Localities for Thermessaite-(NH4)Hide

Showing 3 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
 
  • North Rhine-Westphalia
    • Cologne
      • Aachen
        • Alsdorf
Witzke et al. (2015)
Italy (TL)
 
  • Sicily
    • Metropolitan City of Messina
      • Eolie Islands (Aeolian Islands)
        • Lipari
          • Vulcano Island
Williams et al. (2012) +2 other references
Tajikistan
 
  • Sughd
    • Ayni District
      • Fan-Jagnob coal deposit
Karpenko et al. (2023)
 
and/or  
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