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Efremovite

A valid IMA mineral species
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About EfremoviteHide

09830020017271922766138.jpg
Ivan A. Yefremov
Formula:
(NH4)2Mg2(SO4)3
Colour:
Gray, white
Lustre:
Vitreous, Dull
Hardness:
2
Specific Gravity:
2.52 (Calculated)
Crystal System:
Isometric
Name:
Named in honour of Dr. Ivan Antonovich Yefremov (Ива́н Анто́нович (Анти́пович) Ефре́мов) (22 April 1908, Vyritsa, St. Petersburg, Russian Empire – 5 October 1972, Leningrad, USSR), paleontologist and geologist at the Paleontological Institute, Moscow. He was also a science fiction writer.
Mg analogue of ferroefremovite.

A hygroscopic ammonium magnesium sulphate that hydrates to boussingaultite at room temperature.

Compare also Unnamed (NH4-Mg Sulphate Hydrate).


Unique IdentifiersHide

Mindat ID:
1355
Long-form identifier:
mindat:1:1:1355:6

IMA Classification of EfremoviteHide

Classification of EfremoviteHide

7.AC.10

7 : SULFATES (selenates, tellurates, chromates, molybdates, wolframates)
A : Sulfates (selenates, etc.) without additional anions, without H2O
C : With medium-sized and large cations
28.4.4.3

28 : ANHYDROUS ACID AND NORMAL SULFATES
4 : Miscellaneous
25.3.16

25 : Sulphates
3 : Sulphates of Mg

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

Physical Properties of EfremoviteHide

Vitreous, Dull
Transparency:
Opaque
Comment:
Aggregates dull, presumably vitreous as grains
Colour:
Gray, white
Hardness:
Cleavage:
None Observed
Fracture:
Irregular/Uneven
Density:
2.52 g/cm3 (Calculated)

Optical Data of EfremoviteHide

Type:
Isotropic
RI values:
n = 1.550(1)
Surface Relief:
Low (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

Chemistry of EfremoviteHide

Mindat Formula:
(NH4)2Mg2(SO4)3
Element Weights:
Element% weight
O51.490 %
S25.798 %
Mg13.037 %
N7.513 %
H2.163 %

Calculated from ideal end-member formula.
O
S
Mg
N
H

Crystallography of EfremoviteHide

Crystal System:
Isometric
Class (H-M):
23 - Tetartoidal
Space Group:
P213
Cell Parameters:
a = 9.99(1) Å
Unit Cell V:
997.00 ų (Calculated from Unit Cell)
Z:
4

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
5.76 Å(35)
4.07 Å(70)
3.15 Å(100)
3.00 Å(35)
2.668 Å(50)
1.620 Å(25).

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 10a: Neoproterozoic oxygenation/terrestrial biosphere<0.6
50 : Coal and/or oil shale minerals<0.36
Stage 10b: Anthropogenic minerals<10 Ka
54 : Coal and other mine fire minerals (see also #51 and #56)

Type Occurrence of EfremoviteHide

General Appearance of Type Material:
Equant grains, 0.01-0.015 mm, in gray to white aggregates.
Place of Conservation of Type Material:
Fersman Mineralogical Museum, Academy of Sciences, Moscow.
Geological Setting of Type Material:
From a fumarole at burning dumps at coal mine shafts
Associated Minerals at Type Locality:

Synonyms of EfremoviteHide

Other Language Names for EfremoviteHide

Relationship of Efremovite to other SpeciesHide

Other Members of Langbeinite Group:
CalciolangbeiniteK2Ca2(SO4)3 Iso. 23 : P213
Ferroefremovite(NH4)2Fe2+2(SO4)3Iso. 23 : P213
LangbeiniteK2Mg2(SO4)3Iso. 23 : P213