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Trembathite

A valid IMA mineral species
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About TrembathiteHide

Formula:
Mg3B7O13Cl
Often Fe-bearing; atomic proportion of Fe compared to Mg from approximately 0.32 to 0.5.
Colour:
Colourless to pale blue, dark brown
Lustre:
Vitreous
Hardness:
6 - 8
Specific Gravity:
2.84 - 3.34
Crystal System:
Trigonal
Member of:
Name:
Name after Lowell T. Trembath (1936-1994), Professor of Mineralogy, University of New Brunswick, Fredericton, Canada, for his dedication to mineralogical research and teaching.
Dimorph of:
Boracite Group. The magnesium analogue of congolite, always (at standard temperature and pressure) containing some iron, from Mg0.68Fe0.32 to Mg0.5Fe0.5.

Compare with boracite.


Unique IdentifiersHide

Mindat ID:
4010
Long-form identifier:
mindat:1:1:4010:1

IMA Classification of TrembathiteHide

Classification of TrembathiteHide

6.GA.10

6 : BORATES
G : Heptaborates and other megaborates
A : Tekto-heptaborates
25.6.2.2

25 : ANHYDROUS BORATES CONTAINING HYDROXYL OR HALOGEN
6 : Hexaborates

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

Physical Properties of TrembathiteHide

Vitreous
Transparency:
Transparent
Colour:
Colourless to pale blue, dark brown
Comment:
Dark brown crystals known from the Boulby mine
Streak:
White
Hardness:
6 - 8 on Mohs scale
Fracture:
Conchoidal
Density:
2.84 - 3.34 g/cm3 (Measured)    3.225 g/cm3 (Calculated)

Optical Data of TrembathiteHide

Type:
Uniaxial (-)
RI values:
nω = 1.684(2) nε = 1.668(2)
Max. Birefringence:
δ = 0.016
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.

Surface Relief:
Moderate

Chemistry of TrembathiteHide

Mindat Formula:
Mg3B7O13Cl

Often Fe-bearing; atomic proportion of Fe compared to Mg from approximately 0.32 to 0.5.
Element Weights:
Element% weight
O53.054 %
B19.304 %
Mg18.599 %
Cl9.043 %

Calculated from ideal end-member formula.
Common Impurities:
Mn,Ca

Crystallography of TrembathiteHide

Crystal System:
Trigonal
Class (H-M):
3m - Ditrigonal Pyramidal
Space Group:
R3c
Cell Parameters:
a = 8.588(2) Å, c = 21.050(6) Å
Ratio:
a:c = 1 : 2.451
Unit Cell V:
1,344.52 ų (Calculated from Unit Cell)
Z:
6
Morphology:
Pseudocubic rhombohedra.
Twinning:
Microscopic polysynthetic twinning typical.

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0005564TrembathiteSchindler M, Hawthorne F C (1998) The crystal structure of trembathite, (Mg1.55Fe1.43Mn0.02)B7O13Cl, a mineral of the boracite group: An example of the insertion of a cluster into a three-dimensional net The Canadian Mineralogist 36 1195-120119980293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
3.028 Å(100)
2.050 Å(73)
2.711 Å(66)
2.144 Å(37)
3.497 Å(34)
1.828 Å(25)
2.475 Å(23)

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Near-surface Processes
25 : Evaporites (prebiotic)

Type Occurrence of TrembathiteHide

Synonyms of TrembathiteHide

Other Language Names for TrembathiteHide

Relationship of Trembathite to other SpeciesHide

Member of:
Other Members of Boracite Group:
BoraciteMg3(B7O13)ClOrth. mm2 : Pca21
ChambersiteMn2+3(B7O13)ClOrth. mm2 : Pca21
CongoliteFe2+3B7O13ClTrig. 3m : R3c
EricaiteFe2+3(B7O13)ClOrth. mm2 : Pca21

Common AssociatesHide

Associations Based on Photo Data:
3 photos of Trembathite associated with CongoliteFe2+3B7O13Cl
1 photo of Trembathite associated with SylviteKCl

Related Minerals - Strunz-mindat GroupingHide

6.GA.05EricaiteFe2+3(B7O13)ClOrth. mm2 : Pca21
6.GA.05ChambersiteMn2+3(B7O13)ClOrth. mm2 : Pca21
6.GA.05BoraciteMg3(B7O13)ClOrth. mm2 : Pca21
6.GA.10CongoliteFe2+3B7O13ClTrig. 3m : R3c
6.GA.30KorzhinskiteCa(B2O4) · H2OMon. 2/m : P2/m

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 TrembathiteHide

References for TrembathiteHide

Reference List:

Localities for TrembathiteHide

Showing 5 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.
Canada
 
  • New Brunswick
    • Kings Co.
      • Cardwell Parish
        • Penobsquis
Grice et al. (1996)
      • Hammond Parish
        • Salt Springs evaporite deposit
Burns et al. (1992) +1 other reference
      • Studholm Parish
Grice et al. (2005)
Poland
 
  • Greater Poland Voivodeship
    • Koło County
      • Gmina Kłodawa
PIECZKA et al. (2012) +1 other reference
UK
 
  • England
    • North Yorkshire
      • Redcar and Cleveland
        • Loftus
Schindler et al. (1998) +1 other reference
 
and/or  
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