Epifanovite
A valid IMA mineral species
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About Epifanovite
Formula:
NaCaCu5(PO4)4[AsO2(OH)2] · 7H2O
Colour:
Turquoise blue
Lustre:
Vitreous, Dull
Hardness:
3
Specific Gravity:
3.65
Crystal System:
Monoclinic
Name:
The mineral is named in honor of P. P. Epifanov, Russian geologist and the discoverer of the Kester tin deposit.
The third known mineral to contain phosphate and arsenate (actually dihydroxoarsenate(V)) at separate structural positions (i.e., not substituting for each other) after machatschkiite and walentaite. Considering this separation, the chemical combination in epifanovite is unique among the known (accepted) minerals.
Related to sampleite and andyrobertsite. It may be considered as a more hydrated dihydroxoarsenate equivalent of sampleite.
Epifanovite is structurally close to lavendulan-group minerals (polytypes) and related species: andyrobertsite, calcioandyrobertsite-1M, mahnertite and richelsdorfite.
Related to sampleite and andyrobertsite. It may be considered as a more hydrated dihydroxoarsenate equivalent of sampleite.
Epifanovite is structurally close to lavendulan-group minerals (polytypes) and related species: andyrobertsite, calcioandyrobertsite-1M, mahnertite and richelsdorfite.
Unique Identifiers
Mindat ID:
50773
Long-form identifier:
mindat:1:1:50773:0
IMA Classification of Epifanovite
Approved
IMA Formula:
NaCaCu2+5(PO4)4[As5+O2(OH)2]·7H2O
Approval year:
2016
First published:
2017
Type description reference:
Yakovenchuk, V. N., Pakhomovsky, Ya. A., Konoplyova, N. G., Panikorovskii, T. L., Mikhailova, Yu. A., Bocharov, V. N., Krivovichev, S. V., Ivanyuk, G. Yu. (2018) Epifanovite, NaCaCu5(PO4)4[AsO2(OH)2]·7H2O: a New Mineral from the Kester Deposit, Sakha (Yakutia) Republic, Russia. Geology of Ore Deposits, 60 (7) 587-593 doi:10.1134/s1075701518070103
Classification of Epifanovite
8.CH.70
8 : PHOSPHATES, ARSENATES, VANADATES
C : Phosphates without additional anions, with H2O
H : With large and medium-sized cations, RO4:H2O < 1:1
8 : PHOSPHATES, ARSENATES, VANADATES
C : Phosphates without additional anions, with H2O
H : With large and medium-sized cations, RO4:H2O < 1:1
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 |
|---|---|---|
| Efv | 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 Epifanovite
Vitreous, Dull
Transparency:
Transparent
Comment:
Dull in crusts
Colour:
Turquoise blue
Streak:
Pale blue
Hardness:
3 on Mohs scale
Tenacity:
Brittle
Cleavage:
Perfect
Perfect on (001) and good on (100) and (010)
Perfect on (001) and good on (100) and (010)
Density:
3.65(3) g/cm3 (Measured) 3.73 g/cm3 (Calculated)
Optical Data of Epifanovite
Type:
Biaxial (-)
RI values:
nα = 1.708(5) nβ = 1.730(5) nγ = 1.735(5)
2V:
Measured: 40° to 45°, Calculated: 50°
Max. Birefringence:
δ = 0.027
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:
Moderate
Chemistry of Epifanovite
Mindat Formula:
NaCaCu5(PO4)4[AsO2(OH)2] · 7H2O
Element Weights:
Crystallography of Epifanovite
Crystal System:
Monoclinic
Class (H-M):
2/m - Prismatic
Space Group:
P21/m
Setting:
P21/m
Cell Parameters:
a = 9.6911(8) Å, b = 9.7547(9) Å, c = 9.963(1) Å
β = 102.24(1)°
β = 102.24(1)°
Ratio:
a:b:c = 0.993 : 1 : 1.021
Unit Cell V:
920.43 ų (Calculated from Unit Cell)
Z:
2
Morphology:
Tabular pseudotetragonal crystals up to 50 μm across and 10 μm thick.
X-Ray Powder Diffraction
Powder Diffraction Data:
| d-spacing | Intensity |
|---|---|
| 9.73 Å | (100) |
| 6.79 Å | (35) |
| 4.355 Å | (12) |
| 3.072 Å | (43) |
| 3.061 Å | (24) |
| 3.003 Å | (24) |
| 2.698 Å | (11) |
| 2.405 Å | (10) |
Reference:
Yakovenchuk, V. N., Pakhomovsky, Ya. A., Konoplyova, N. G., Panikorovskii, T. L., Mikhailova, Yu. A., Bocharov, V. N., Krivovichev, S. V., Ivanyuk, G. Yu. (2018) Epifanovite, NaCaCu5(PO4)4[AsO2(OH)2]·7H2O: a New Mineral from the Kester Deposit, Sakha (Yakutia) Republic, Russia. Geology of Ore Deposits, 60 (7) 587-593 doi:10.1134/s1075701518070103
Geological Environment
Paragenetic Mode(s):
| Paragenetic Mode | Earliest Age (Ga) |
|---|---|
| Stage 7: Great Oxidation Event | <2.4 |
| 47a : [Near-surface hydration of prior minerals] | |
| 47c : [Carbonates, phosphates, borates, nitrates] | |
| 47d : [Arsenates, antimonates, selenates, bismuthinates] |
Type Occurrence of Epifanovite
General Appearance of Type Material:
Crusts of tabular pseudo-tetragonal crystals up to 50 µm across and 10 μm thick.
Place of Conservation of Type Material:
Collections of the Mineralogical Museum of the St. Petersburg State University, Russia (catalogue No. 19658/1)
Empirical Formula of Type Material:
(Na0.94K0.06)Σ1.00Ca0.82Na0.08)Σ0.90(Cu5.04Zn0.06)Σ5.10(PO4)4[(As0.81P0.19)Σ1.00(O1.92OH2.06Cl0.02)Σ4.00]7.37H2O
Geological Setting of Type Material:
It was found in a quartz-phosphate nest within greisenized cassiterite-rich grano-diorite of the Kester tin deposit
Associated Minerals at Type Locality:
Reference:
Yakovenchuk, V. N., Pakhomovsky, Ya. A., Konoplyova, N. G., Panikorovskii, T. L., Mikhailova, Yu. A., Bocharov, V. N., Krivovichev, S. V., Ivanyuk, G. Yu. (2018) Epifanovite, NaCaCu5(PO4)4[AsO2(OH)2]·7H2O: a New Mineral from the Kester Deposit, Sakha (Yakutia) Republic, Russia. Geology of Ore Deposits, 60 (7) 587-593 doi:10.1134/s1075701518070103
Synonyms of Epifanovite
Other Language Names for Epifanovite
Dutch:Epifanoviet
German:Epifanovit
Common Associates
Associations Based on Photo Data:
| 2 photos of Epifanovite associated with Fluorapatite | Ca5(PO4)3F |
| 2 photos of Epifanovite associated with Native Copper | Cu |
| 1 photo of Epifanovite associated with Pseudomalachite | Cu5(PO4)2(OH)4 |
| 1 photo of Epifanovite associated with Sergeysmirnovite | MgZn2(PO4)2 · 4H2O |
Related Minerals - Strunz-mindat Grouping
| 8.CH.05 | Natrowalentaite | [Fe3+0.5Na0.5(H2O)6][NaAs3+2(Fe3+2.33W6+0.67)(PO4)2O7] |
| 8.CH.05 | Walentaite | [Mn2+(H2O)6][◻As3+3Fe3+3(PO4)2O7] |
| 8.CH.05 | Halilsarpite | [Mg(H2O)6][CaAs3+2(Fe3+2.67Mo6+0.33)(AsO4)2O7] |
| 8.CH.10 | Anapaite | Ca2Fe2+(PO4)2 · 4H2O |
| 8.CH.15 | Picropharmacolite | Ca4Mg(AsO4)2(HAsO4)2 · 11H2O |
| 8.CH.20 | Dittmarite | (NH4)Mg(PO4) · H2O |
| 8.CH.20 | Niahite | (NH4)Mn2+(PO4) · H2O |
| 8.CH.25 | Taranakite | K3Al5(PO3OH)6(PO4)2 · 18H2O |
| 8.CH.25 | Francoanellite | K3Al5(PO3OH)6(PO4)2 · 12H2O |
| 8.CH.25 | Macivorite | (NH4)3Al5(PO3OH)6(PO4)2 · 18H2O |
| 8.CH.30 | Schertelite | (NH4)2MgH2(PO4)2 · 4H2O |
| 8.CH.35 | Hannayite | (NH4)2Mg3H4(PO4)4 · 8H2O |
| 8.CH.40 | Hazenite | KNaMg2(PO4)2 · 14H2O |
| 8.CH.40 | Struvite-(K) | KMg(PO4) · 6H2O |
| 8.CH.40 | Struvite | (NH4)Mg(PO4) · 6H2O |
| 8.CH.45 | Rimkorolgite | (Mg,Mn)5(Ba,Sr,Ca)(PO4)4 · 8H2O |
| 8.CH.50 | Bakhchisaraitsevite | Na2Mg5(PO4)4 · 7H2O |
| 8.CH.55 | Smolyaninovite | Co3Fe3+2(AsO4)4 · 11H2O |
| 8.CH.55 | Fahleite | CaZn5Fe3+2(AsO4)6 · 14H2O |
| 8.CH.60 | Barahonaite-(Fe) | (Ca,Cu,Na,Fe3+,Al)12Fe3+2(AsO4)8(OH,Cl)x · nH2O |
| 8.CH.60 | Barahonaite-(Al) | (Ca,Cu,Na,Fe3+,Al)12Al2(AsO4)8(OH,Cl)x · nH2O |
| 8.CH.75 | Esdanaite-(Ce) | NaMnCe(PO4)2 · 4H2O |
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 Epifanovite
mindat.org URL:
https://www.mindat.org/min-50773.html
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References for Epifanovite
Reference List:
Hålenius, U., Hatert, F., Pasero, M., Mills, S. J. (2016) New minerals and nomenclature modifications approved in 2016, CNMNC Newsletter No 34. Mineralogical Magazine, 80 (7) 1315-1321 doi:10.1180/minmag.2016.080.086
Yakovenchuk, V. N., Pakhomovsky, Ya. A., Konoplyova, N. G., Panikorovskii, T. L., Mikhailova, Yu. A., Bocharov, V. N., Krivovichev, S. V., Ivanyuk, G. Yu. (2018) Epifanovite, NaCaCu5(PO4)4[AsO2(OH)2]·7H2O: a New Mineral from the Kester Deposit, Sakha (Yakutia) Republic, Russia. Geology of Ore Deposits, 60 (7) 587-593 doi:10.1134/s1075701518070103
Localities for Epifanovite
Showing 1 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.
Russia (TL) | |
| Hålenius et al. (2016) +2 other references |
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The
Kester deposit, Kester harpolith, Arga-Ynnakh-Khaya granite Massif, Yana-Adycha Region, Yana River Basin, Verkhoyansk District, Sakha, Russia