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Novograblenovite

A valid IMA mineral species
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Prokopiy T. Novograblenov
Formula:
(NH4)MgCl3 · 6H2O
Colour:
Colorless
Lustre:
Vitreous
Hardness:
1 - 2
Specific Gravity:
1.504 (Calculated)
Crystal System:
Monoclinic
Name:
Named in honor of Prokopiy Trifonovich Novograblenov (Прокопий Трифонович Новограбленов) (14 August 1892, Petropavlovsk, Russian Empire – 1 January 1934, Petropavlovsk, USSR), one of the researchers of the Kamchatka Peninsula, a teacher, naturalist, geographer, and geologist, and author of the most important catalogue of volcanoes on the Kamchatka Peninsula.
Dimorph of:
Structurally and chemically related to carnallite. Compare 'redikortsevite'.


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Unique IdentifiersHide

Mindat ID:
52169
Long-form identifier:
mindat:1:1:52169:7

IMA Classification of NovograblenoviteHide

Classification of NovograblenoviteHide

3.BA.15

3 : HALIDES
B : Simple halides, with H2O
A : M:X = 1:1 and 2:3

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

Physical Properties of NovograblenoviteHide

Vitreous
Transparency:
Transparent
Colour:
Colorless
Streak:
White
Hardness:
1 - 2 on Mohs scale
Tenacity:
Brittle
Cleavage:
None Observed
Parting:
Not observed
Comment:
Thin needles are flexible, fracture is described as even
Density:
1.504 g/cm3 (Calculated)
Comment:
Calculated from empirical formula

Optical Data of NovograblenoviteHide

Type:
Biaxial (+)
RI values:
nα = 1.469(2) nβ = 1.479(2) nγ = 1.496(2)
2V:
Measured: 80° (10), Calculated: 75.7°
Max. Birefringence:
δ = 0.027
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:
Moderate (negative)
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.
Dispersion:
Very weak, r > v
Pleochroism:
Non-pleochroic
Comments:
c^Z = 40°

Chemistry of NovograblenoviteHide

Mindat Formula:
(NH4)MgCl3 · 6H2O
Element Weights:
Element% weight
Cl41.418 %
O37.383 %
Mg9.465 %
H6.280 %
N5.454 %

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

Crystallography of NovograblenoviteHide

Crystal System:
Monoclinic
Class (H-M):
2/m - Prismatic
Space Group:
B2/b
Setting:
C2/c
Cell Parameters:
a = 9.2734(3) Å, b = 9.5176(3) Å, c = 13.2439(4) Å
β = 90.187(2)°
Ratio:
a:b:c = 0.974 : 1 : 1.392
Unit Cell V:
1168.91 ų
Z:
4

X-Ray Powder DiffractionHide

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Stage 7: Great Oxidation Event<2.4
45b : [Other oxidized fumarolic minerals]

Type Occurrence of NovograblenoviteHide

Synonyms of NovograblenoviteHide

Other Language Names for NovograblenoviteHide

Related Minerals - Strunz-mindat GroupingHide

3.BA.05HydrohaliteNaCl · 2H2OMon. 2/m : P21/c
3.BA.10CarnalliteKMgCl3 · 6H2OOrth. mmm(2/m2/m2/m) : Pnna
3.BA.20CryobostryxiteKZnCl3 · 2H2OMon. 2/m : P21/c

Fluorescence of NovograblenoviteHide

Other InformationHide

Thermal Behaviour:
Two-step dehydration at 155 and 193°C and sublimation of NH4Cl at 341°C.
Notes:
Soluble in water, alcohol, and acetone; it dissolves in hydrochloric acid without gas evolution.
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 NovograblenoviteHide

References for NovograblenoviteHide

Localities for NovograblenoviteHide

Showing 2 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.
Russia (TL)
 
  • Kamchatka Krai
    • Milkovsky District
      • Tolbachik Volcanic field
        • Plosky Tolbachik Volcano
Okrugin et al. (2019)
The Moon
 
  • Oceanus Procellarum (Ocean of Storms)
Jin et al. (2024)
 
and/or  
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