Krinovite
A valid IMA mineral species
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Formula:
Na2Mg4Cr3+2(Si6O18)O2
Colour:
Emerald green
Lustre:
Sub-Adamantine
Hardness:
5½ - 7
Specific Gravity:
3.38
Crystal System:
Triclinic
Member of:
Name:
Named in honor of Evgeny Leonidovich Krinov (Евгений Леонидович Кринов) (3 March 1906, Tambov, Russian Empire - 2 January 1984), Russian expert on meteorites. It is pronounced kreen'-off-ite.
This page provides mineralogical data about Krinovite.
Unique Identifiers
Mindat ID:
2276
Long-form identifier:
mindat:1:1:2276:3
Similar Names
| Greenovite | A variety of Titanite | (Ca,Mn)Ti(SiO4)O |
| Khrenovite | A valid IMA mineral species | Na3Fe23+(AsO4)3 |
IMA Classification of Krinovite
Approved
IMA Formula:
Na4(Mg8Cr3+4)O4[Si12O36]
Approval year:
1967
First published:
1968
Classification of Krinovite
9.DH.40
9 : SILICATES (Germanates)
D : Inosilicates
H : Inosilicates with 4-periodic single chains, Si4O12
9 : SILICATES (Germanates)
D : Inosilicates
H : Inosilicates with 4-periodic single chains, Si4O12
69.2.1a.4
69 : INOSILICATES Chains with Side Branches or Loops
2 : Chains with Side Branches or Loops with P>2
69 : INOSILICATES Chains with Side Branches or Loops
2 : Chains with Side Branches or Loops with P>2
14.15.4
14 : Silicates not Containing Aluminum
15 : Silicates of Cr
14 : Silicates not Containing Aluminum
15 : Silicates of Cr
Mineral Symbols
As of 2021 there are now IMA–CNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.
| Symbol | Source | Reference for Standard |
|---|---|---|
| Kvi | IMA–CNMNC | Warr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43 |
Physical Properties of Krinovite
Sub-Adamantine
Transparency:
Translucent
Colour:
Emerald green
Streak:
Greenish white
Hardness:
5½ - 7 on Mohs scale
Cleavage:
None Observed
Density:
3.38 g/cm3 (Measured) 3.44 g/cm3 (Calculated)
Optical Data of Krinovite
Type:
Biaxial (+)
RI values:
nα = 1.712 nβ = 1.725 nγ = 1.76
2V:
Measured: 61° , Calculated: 64°
Max. Birefringence:
δ = 0.048
Based on recorded range of RI values above.
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.
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).
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.
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:
relatively strong
Pleochroism:
Strong
Comments:
X = yellow-green; Y = blue-green; Z = greenish black, may be an anomalous dark reddish brown
Chemistry of Krinovite
Mindat Formula:
Na2Mg4Cr3+2(Si6O18)O2
Element Weights:
Common Impurities:
Ti,Al,Fe,Mn,Ca,K
Crystallography of Krinovite
Crystal System:
Triclinic
Class (H-M):
1 - Pinacoidal
Space Group:
P1
Cell Parameters:
a = 10.23 Å, b = 10.64 Å, c = 8.78 Å
α = 105.15°, β = 96.5°, γ = 125.15°
α = 105.15°, β = 96.5°, γ = 125.15°
Ratio:
a:b:c = 0.961 : 1 : 0.825
Unit Cell V:
710.91 ų (Calculated from Unit Cell)
Z:
2
Twinning:
Multiple twinning common.
Crystal Structure
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Unit Cell | Unit Cell Packed
2x2x2 | 3x3x3 | 4x4x4
Unit Cell | Unit Cell Packed
2x2x2 | 3x3x3 | 4x4x4
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CIF File Best | x | y | z | a | b | c
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Data courtesy of the American Mineralogist Crystal Structure Database. Click on an AMCSD ID to view structure
| ID | Species | Reference | Link | Year | Locality | Pressure (GPa) | Temp (K) |
|---|---|---|---|---|---|---|---|
| 0010992 | Krinovite | Bonaccorsi E, Merlino S, Pasero M (1989) The crystal structure of the meteoritic mineral krinovite, NaNaMg2CrSi3O10 Zeitschrift fur Kristallographie 187 133-138 | ![]() | 1989 | Wichita County, USA | 0 | 293 |
CIF Raw Data - click here to close
X-Ray Powder Diffraction
Powder Diffraction Data:
| d-spacing | Intensity |
|---|---|
| 2.501 Å | (100) |
| 2.655 Å | (90) |
| 2.893 Å | (80) |
| 2.080 Å | (70) |
| 7.92 Å | (60) |
| 3.639 Å | (60) |
| 3.104 Å | (60) |
Geological Environment
Paragenetic Mode(s):
| Paragenetic Mode | Earliest Age (Ga) |
|---|---|
| Stage 2: Planetesimal differentiation and alteration | 4.566-4.550 |
| 5 : Primary asteroid phases | 4.566–4.560 |
Type Occurrence of Krinovite
Geological Setting of Type Material:
octahedrite iron meteorites
Associated Minerals at Type Locality:
Synonyms of Krinovite
Other Language Names for Krinovite
Relationship of Krinovite to other Species
Member of:
Other Members of Aenigmatite Group:
| Aenigmatite | Na4[Fe2+10Ti2]O4[Si12O36] | Tric. 1 : P1 |
| 'UM1991-29-SiO:FeMgNa' | Na4(Mg5Fe3+7)O4[Si9Fe3+3O36] | |
| Wilkinsonite | Na2Fe2+4Fe3+2(Si6O18)O2 | Tric. 1 : P1 |
Related Minerals - Strunz-mindat Grouping
| 9.DH. | Devilliersite | Ca4Ca2Fe3+10O4[(Fe3+10Si2)O36] |
| 9.DH. | 'Gageite-2M' | (Mn,Mg,Zn)42Si16O54(OH)40 |
| 9.DH. | Bavsiite | Ba2V2O2[Si4O12] |
| 9.DH. | Yuzuxiangite | Sr3Fe3+(Si2O6)2(OH) · 3H2O |
| 9.DH. | Louisfuchsite | Ca2(Mg4Ti2)(Al4Si2)O20 |
| 9.DH.05 | Leucophanite | NaCaBeSi2O6F |
| 9.DH.10 | Ohmilite | Sr3(Ti,Fe3+)(Si4O12)(O,OH) · 2-3H2O |
| 9.DH.15 | Haradaite | SrVSi2O7 |
| 9.DH.15 | Suzukiite | BaVSi2O7 |
| 9.DH.20 | Shcherbakovite | (K,Ba)KNa(Ti,Nb)2(Si4O12)O2 |
| 9.DH.20 | Batisite | BaNaNaTi2(Si4O12)O2 |
| 9.DH.20 | Noonkanbahite | BaKNaTi2(Si4O12)O2 |
| 9.DH.25 | Taikanite | Sr3BaMn2+2(Si4O12)O2 |
| 9.DH.30 | Krauskopfite | BaSi2O5 · 3H2O |
| 9.DH.35 | Gageite | Mn21(Si4O12)2O3(OH)20 |
| 9.DH.35 | Balangeroite | (Mg,Fe2+,Fe3+,Mn2+)42Si16O54(OH)40 |
| 9.DH.40 | Kuratite | Ca2(Fe2+5Ti)O2[Si4Al2O18] |
| 9.DH.40 | Aenigmatite | Na4[Fe2+10Ti2]O4[Si12O36] |
| 9.DH.40 | Dorrite | Ca4(Mg3Fe3+9)O4(Si3Al8Fe3+O36) |
| 9.DH.40 | Serendibite | Ca4[Mg6Al6]O4[Si6B3Al3O36] |
| 9.DH.40 | Rhönite | Ca4[Mg8Fe3+2Ti2]O4[Si6Al6O36] |
| 9.DH.40 | Khesinite | Ca4(Mg3Fe3+9)O4(Fe3+9Si3)O36 |
| 9.DH.40 | 'UM1991-29-SiO:FeMgNa' | Na4(Mg5Fe3+7)O4[Si9Fe3+3O36] |
| 9.DH.40 | Høgtuvaite | Ca4[Fe2+6Fe3+6]O4[Si8Be2Al2O36] |
| 9.DH.40 | 'Leucorhönite' | Ca2(Mg,Fe3+,Al)6(Si,Al)6O20 |
| 9.DH.40 | Welshite | Ca4Mg9Sb3O4[Si6Be3AlFe2O36] |
| 9.DH.40 | Wilkinsonite | Na2Fe2+4Fe3+2(Si6O18)O2 |
| 9.DH.40 | Makarochkinite | (Ca,Na)4[Fe2+8Fe3+2Ti2]O4[Si8Be2Al2O36] |
| 9.DH.45 | Sapphirine | Mg4(Mg3Al9)O4[Si3Al9O36] |
| 9.DH.50 | Khmaralite | (Mg,Al,Fe)16[(Al,Si,Be)12O36]O4 |
| 9.DH.55 | 'UM1988-26-SiO:AlMg' | Mg4Al2O[Si3Al2O15] |
| 9.DH.55 | Surinamite | (Mg,Fe)3Al4BeSi3O16 |
| 9.DH.60 | Deerite | Fe2+6Fe3+3(Si6O17)O3(OH)5 |
| 9.DH.65 | Taneyamalite | (Na,Ca)Mn2+12(Si,Al)12(O,OH)44 |
| 9.DH.65 | Howieite | Na(Fe2+,Fe3+,Al,Mg)12(Si6O17)2(O,OH)10 |
| 9.DH.70 | Johninnesite | Na2Mn2+9Mg7(OH)8[AsO4]2[Si6O17]2 |
| 9.DH.75 | Agrellite | NaCa2Si4O10F |
Other Information
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 Krinovite
mindat.org URL:
https://www.mindat.org/min-2276.html
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Please feel free to link to this page.
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References for Krinovite
Reference List:
Olsen, E., Fuchs, L. (1968) Krinovite, NaMg2CrSi3O10: A New Meteorite Mineral. Science, 161 (3843). 786-787 doi:10.1126/science.161.3843.786
Merlino, S. (1972) X-ray crystallography of krinovite. Zeitschrift für Kristallographie: 136: 81-88.
Bonaccorsi, Elena, Merlino, Stefano, Pasero, Marco (1989) The crystal structure of the meteoritic mineral krinovite, NaMg2CrSi3O10. Zeitschrift für Kristallographie - Crystalline Materials, 187 (1) 133-138 doi:10.1524/zkri.1989.187.1-2.133
Jensen, B. B. (1996) Solid solution among members of the aenigmatite group. Mineralogical Magazine, 60 (403) 982-986 doi:10.1180/minmag.1996.060.403.14
Localities for Krinovite
Showing 5 localities.
Locality List
- 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).
All localities listed without proper references should be considered as questionable.
Australia | |
| Merlino (1972) |
Mexico | |
| Meteoritical Bulletin: MB 107 (2018) |
Poland | |
| Galuskin et al. (2026) |
USA (TL) | |
| Olsen et al. (1968) +3 other references |
| rruff.geo.arizona.edu (n.d.) |
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