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Väyrynenite

A valid IMA mineral species - grandfathered
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About VäyryneniteHide

03371800017271927637779.jpg
Heikki A. Väyrynen
Formula:
BeMn2+(PO4)(OH)
May contain minor F substituting for OH.
Colour:
Light pink to rose-red, salmon pink, pale gray, brown
Lustre:
Vitreous
Hardness:
5
Specific Gravity:
3.22
Crystal System:
Monoclinic
Name:
Named after Heikki Allan Väyrynen (18 May 1888, Pielisjärvi, Finland - 29 August 1956), professor of mineralogy, Technical University, Helsinki (Finland).
The manganese-beryllium-phosphate väyrynenite was first recognized in 1939 as a possible new mineral by Oleg von Knorring (1915-1994). However, it was first described as a new mineral by Volborth (1954), from Viitaniemi, Eräjärvi, Finland. Additional mineralogical data and a new chemical analysis were given by Mrose and von Knorring (1959).


Name EncodingHide

ASCII-7:
Vayrynenite

Unique IdentifiersHide

Mindat ID:
4220
Long-form identifier:
mindat:1:1:4220:4

IMA Classification of VäyryneniteHide

Approved, 'Grandfathered' (first described prior to 1959)
IMA Formula:
Mn2+Be(PO4)OH
First published:
1954

Classification of VäyryneniteHide

8.BA.05

8 : PHOSPHATES, ARSENATES, VANADATES
B : Phosphates, etc., with additional anions, without H2O
A : With small and medium-sized cations
41.5.4.3

41 : ANHYDROUS PHOSPHATES, ETC.CONTAINING HYDROXYL OR HALOGEN
5 : (AB)2(XO4)Zq
22.1.20

22 : Phosphates, Arsenates or Vanadates with other Anions
1 : Phosphates, arsenates or vanadates with fluoride

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

Physical Properties of VäyryneniteHide

Vitreous
Transparency:
Transparent, Translucent
Colour:
Light pink to rose-red, salmon pink, pale gray, brown
Streak:
White
Hardness:
Tenacity:
Brittle
Cleavage:
Perfect
Perfect {010}, good {100}, fair {001}.
Fracture:
Irregular/Uneven
Density:
3.22 g/cm3 (Measured)    3.23 g/cm3 (Calculated)

Optical Data of VäyryneniteHide

Type:
Biaxial (-)
RI values:
nα = 1.638 - 1.64 nβ = 1.658 - 1.662 nγ = 1.664 - 1.667
2V:
Measured: 46° to 55°, Calculated: 51° to 57°
Max. Birefringence:
δ = 0.026 - 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:
High (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
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:
r > v moderate
Pleochroism:
Visible
Comments:
X= orangish
Y= red
Z= dark red

Chemistry of VäyryneniteHide

Mindat Formula:
BeMn2+(PO4)(OH)

May contain minor F substituting for OH.
Element Weights:
Element% weight
O45.471 %
Mn31.227 %
P17.606 %
Be5.123 %
H0.573 %

Calculated from ideal end-member formula.
O
Mn
P
Be
H
Common Impurities:
F

Chemical AnalysisHide

Oxide wt%:
 1
MnO34.01 %
FeO5.92 %
CaO0.53 %
BeO13.85 %
Na2O0.20 %
K2O0.04 %
Al2O30.40 %
Li2Otraces %
P2O539.98 %
H2O+4.93 %
H2O-0.19 %
F0.00 %
insol.0.06 %
Total:100.11 %

Crystallography of VäyryneniteHide

Crystal System:
Monoclinic
Class (H-M):
2/m - Prismatic
Space Group:
P21/b
Cell Parameters:
a = 5.4044(6) Å, b = 14.5145(12) Å, c = 4.7052(6) Å
β = 102.798(9)°
Ratio:
a:b:c = 0.372 : 1 : 0.324
Unit Cell V:
359.91 ų
Z:
4
Morphology:
Often as fine grained aggregates. Euhedral crystals are rare. Short to long prismatic crystals parallel to [001]. Forms observed: {001}, prisms {010} and {110}. Prism faces are generally striated vertically
Comment:
Huminicki and Hawthorne (2000)

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
3.452 Å(100)
7.251 Å(85)
2.885 Å(85)
4.399 Å(60)
2.662 Å(42)
2.951 Å(35)
4.960 Å(25)
Comments:
Viitaniemi pegmatite, Finland. Data from Mrose and Von Knorring (1959).

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Near-surface Processes
22 : Hydration and low-? subsurface aqueous alteration (see also #23)
Geological Setting:
Alteration product of beryl and triphylite in complex granitic pegmatites.

Type Occurrence of VäyryneniteHide

Place of Conservation of Type Material:
National Museum of Natural History, Washington, D.C., USA, number R11807 (type).
Geological Setting of Type Material:
Granite pegmatite.
Associated Minerals at Type Locality:

Synonyms of VäyryneniteHide

Other Language Names for VäyryneniteHide

Simplified Chinese:红磷锰铍石
Spanish:Väyrynenita

Common AssociatesHide

Associations Based on Photo Data:
24 photos of Väyrynenite associated with 'Cleavelandite'Na(AlSi3O8)
24 photos of Väyrynenite associated with TopazAl2(SiO4)(F,OH)2
21 photos of Väyrynenite associated with EosphoriteMn2+Al(PO4)(OH)2 · H2O
16 photos of Väyrynenite associated with MuscoviteKAl2(AlSi3O10)(OH)2
14 photos of Väyrynenite associated with QuartzSiO2
11 photos of Väyrynenite associated with HurlbutiteCaBe2(PO4)2
11 photos of Väyrynenite associated with 'Indicolite'
11 photos of Väyrynenite associated with SchorlNaFe2+3Al6(Si6O18)(BO3)3(OH)3(OH)
9 photos of Väyrynenite associated with TourmalineAD3G6(T6O18)(BO3)3X3Z
8 photos of Väyrynenite associated with Tantalite-(Mn)Mn2+Ta2O6

Related Minerals - Strunz-mindat GroupingHide

8.BA.Vladkuzminite K4CuZn3(AsO4)4Mon. 2/m : P21/b
8.BA.AxeliteNa14Cu7(AsO4)8F2Cl2Tet. 4mm : P4bm
8.BA.Elramlyite-(Ce)(◻0.67Ce0.33)Th2(PO4)2F3Mon. 2/m
8.BA.Tomcampbellite[KCl][Fe2+14(OH)6(PO4)6(PO3OH)2]Mon. 2/m : B2/m
8.BA.10HerderiteCaBe(PO4)FMon. 2/m
8.BA.10BergslagiteCaBeAsO4(OH)Mon. 2/m : P21/b
8.BA.10HydroxylherderiteCaBe(PO4)(OH)Mon. 2/m : P21/b
8.BA.15BabefphiteBaBePO4(F,OH)Tric. 1 : P1

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 VäyryneniteHide

References for VäyryneniteHide

Reference List:

Localities for VäyryneniteHide

Showing 20 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.
Afghanistan
 
  • Nuristan
    • Kamdesh District
Niedermayr (2001) +1 other reference
China
 
  • Fujian
    • Nanping
      • Yanping District
        • Nanping pegmatite field
Yueqing Yang et al. (1987) +3 other references
Finland
 
  • Pirkanmaa
    • Orivesi
      • Eräjärvi area
Lahti (1981)
Volborth (1954) +5 other references
Kazakhstan
 
  • East Kazakhstan Region
    • Ulan District
Gordiyenko et al. (1973) +1 other reference
Nigeria
 
Dr. Wing Tak Lui collection
Pakistan
 
  • Gilgit-Baltistan
    • Roundu District
Moore (2005)
    • Shigar District
      • Braldu Valley
        • Dassu
Blauwet (2006)
H. Obodda
imported from Shigar District +2 other references
  • Khyber Pakhtunkhwa Province
    • Chitral District
      • Lower Chitral District
Meixner & Paar (1976)
Portugal
 
  • Guarda
    • Sabugal
      • Bendada
Schnorrer-Köhler et al. (1991)
Russia
 
  • Zabaykalsky Krai
    • Ononsky District
      • Durulgui granite-pegmatite system
Lykova I. S. et al. (2017)
Spain
 
  • Castile and Leon
    • Salamanca
Roda Robles et al. (1999) +1 other reference
Sweden
 
  • Stockholm County
    • Haninge
      • Norrö
Nysten et al. (2006)
    • Sigtuna
      • Arlanda
Langhof et al. (2016)
USA
 
  • Maine
    • Cumberland County
      • Baldwin
        • West Baldwin
A.U. Falster et al. (2011)
    • Oxford County
      • Greenwood
        • Uncle Tom Mountain
Falster et al. (2019) +1 other reference
King et al. (1994) +1 other reference
  • Wisconsin
    • Florence County
      • Fern
        • Pine River pegmatites
Falster et al. (1996)
 
and/or  
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