Fayalite
A valid IMA mineral species - grandfathered
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About Fayalite
Formula:
Fe2+2(SiO4)
Colour:
Greenish-yellow, yellow or brown
Lustre:
Vitreous, Greasy
Hardness:
7
Specific Gravity:
4.39
Crystal System:
Orthorhombic
Member of:
Name:
Named by Christian Gottlieb Gmelin in 1840 for the type locality, Faial Island (Fayal Island), Azores District (Azores Islands), Portugal.
Type Locality:
Isostructural with:
Olivine Group. Fayalite-Forsterite Series, and the Fayalite-Tephroite Series. The Fe2+ analogue of Forsterite, Tephroite, and Calcio-Olivine.
Uncommon in nature, but common in man-made (metallurgy) iron slags.
See also laihunite.
Visit gemdat.org for gemological information about Fayalite.
Uncommon in nature, but common in man-made (metallurgy) iron slags.
See also laihunite.
Visit gemdat.org for gemological information about Fayalite.Unique Identifiers
Mindat ID:
1458
Long-form identifier:
mindat:1:1:1458:4
IMA Classification of Fayalite
Approved, 'Grandfathered' (first described prior to 1959)
IMA Formula:
Fe2+2SiO4
Classification of Fayalite
9.AC.05
9 : SILICATES (Germanates)
A : Nesosilicates
C : Nesosilicates without additional anions; cations in octahedral [6] coordination
9 : SILICATES (Germanates)
A : Nesosilicates
C : Nesosilicates without additional anions; cations in octahedral [6] coordination
51.3.1.1
51 : NESOSILICATES Insular SiO4 Groups Only
3 : Insular SiO4 Groups Only with all cations in octahedral [6] coordination
51 : NESOSILICATES Insular SiO4 Groups Only
3 : Insular SiO4 Groups Only with all cations in octahedral [6] coordination
14.19.1
14 : Silicates not Containing Aluminum
19 : Silicates of Fe
14 : Silicates not Containing Aluminum
19 : Silicates of Fe
Mineral Symbols
As of 2021 there are now IMA–CNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.
Please only use the official IMA–CNMNC symbol. Older variants are listed for historical use only.
Please only use the official IMA–CNMNC symbol. Older variants are listed for historical use only.
| Symbol | Source | Reference for Standard |
|---|---|---|
| Fa | IMA–CNMNC | Warr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43 |
| Fa | Kretz (1983) | Kretz, R. (1983) Symbols of rock-forming minerals. American Mineralogist, 68, 277–279. |
| Fa | Siivolam & Schmid (2007) | Siivolam, J. and Schmid, R. (2007) Recommendations by the IUGS Subcommission on the Systematics of Metamorphic Rocks: List of mineral abbreviations. Web-version 01.02.07. IUGS Commission on the Systematics in Petrology. download |
| Fa | Whitney & Evans (2010) | Whitney, D.L. and Evans, B.W. (2010) Abbreviations for names of rock-forming minerals. American Mineralogist, 95, 185–187 doi:10.2138/am.2010.3371 |
| Fa | The Canadian Mineralogist (2019) | The Canadian Mineralogist (2019) The Canadian Mineralogist list of symbols for rock- and ore-forming minerals (December 30, 2019). download |
Physical Properties of Fayalite
Vitreous, Greasy
Transparency:
Transparent, Translucent
Colour:
Greenish-yellow, yellow or brown
Streak:
Colourless
Hardness:
7 on Mohs scale
Density:
4.39 g/cm3 (Measured)
Comment:
measured on synthetic material
Optical Data of Fayalite
Type:
Biaxial (-)
RI values:
nα = 1.731 - 1.824 nβ = 1.76 - 1.864 nγ = 1.773 - 1.875
2V:
Measured: 74° to 47°, Calculated: 54° to 66°
Max. Birefringence:
δ = 0.042 - 0.051
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:
weak
Pleochroism:
Visible
Comments:
X = pale yellow
Y = orange-yellow, reddish-brown
Z = pale yellow
Y = orange-yellow, reddish-brown
Z = pale yellow
Chemistry of Fayalite
Mindat Formula:
Fe2+2(SiO4)
Element Weights:
Elements listed:
Common Impurities:
Mn,Mg
Crystallography of Fayalite
Crystal System:
Orthorhombic
Class (H-M):
mmm(2/m2/m2/m) - Dipyramidal
Cell Parameters:
a = 4.79 Å, b = 10.39 Å, c = 6.06 Å
Ratio:
a:b:c = 0.461 : 1 : 0.583
Unit Cell V:
301.59 ų (Calculated from Unit Cell)
Z:
4
Comment:
Space group Pbnm (non-standard setting).
Crystal Structure
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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) |
|---|---|---|---|---|---|---|---|
| 0000332 | Fayalite | Smyth J R, Hazen R M (1973) The crystal structures of forsterite and hortonolite at several temperatures up to 900 C American Mineralogist 58 588-593 | ![]() | 1973 | Franklin, New Jersey, USA | 0 | 298 |
| 0019699 | Fayalite | Redfern S A T, Knight K S, Henderson C M B, Wood B J (1998) Fe-Mn cation ordering in fayalite-tephroite (FexMn1-x)2SiO4 olivines: A neutron diffraction study Mineralogical Magazine 62 607-615 | ![]() | 1998 | synthetic | 0 | 293 |
| 0019698 | Fayalite | Redfern S A T, Knight K S, Henderson C M B, Wood B J (1998) Fe-Mn cation ordering in fayalite-tephroite (FexMn1-x)2SiO4 olivines: A neutron diffraction study Mineralogical Magazine 62 607-615 | ![]() | 1998 | synthetic | 0 | 293 |
| 0009731 | Fayalite | Fujino K, Sasaki S, Takeuchi Y, Sadanaga R (1981) X-ray determination of electron distributions in forsterite, fayalite and tephroite Acta Crystallographica B37 513-518 | ![]() | 1981 | synthetic | 0 | 293 |
| 0000570 | Fayalite | Hazen R M (1977) Effects of temperature and pressure on the crystal structure of ferromagnesian olivine American Mineralogist 62 286-295 | ![]() | 1977 | Franklin, New Jersey, USA | 0 | 293 |
| 0000569 | Fayalite | Hazen R M (1977) Effects of temperature and pressure on the crystal structure of ferromagnesian olivine American Mineralogist 62 286-295 | ![]() | 1977 | synthetic | 0 | 293 |
| 0000568 | Fayalite | Hazen R M (1977) Effects of temperature and pressure on the crystal structure of ferromagnesian olivine American Mineralogist 62 286-295 | ![]() | 1977 | synthetic | 0 | 293 |
| 0000567 | Fayalite | Hazen R M (1977) Effects of temperature and pressure on the crystal structure of ferromagnesian olivine American Mineralogist 62 286-295 | ![]() | 1977 | synthetic | 0 | 293 |
| 0000566 | Fayalite | Hazen R M (1977) Effects of temperature and pressure on the crystal structure of ferromagnesian olivine American Mineralogist 62 286-295 | ![]() | 1977 | synthetic | 0 | 293 |
| 0000565 | Fayalite | Hazen R M (1977) Effects of temperature and pressure on the crystal structure of ferromagnesian olivine American Mineralogist 62 286-295 | ![]() | 1977 | synthetic | 0 | 77 |
| 0000571 | Fayalite | Hazen R M (1977) Effects of temperature and pressure on the crystal structure of ferromagnesian olivine American Mineralogist 62 286-295 | ![]() | 1977 | Franklin, New Jersey, USA | 0 | 573 |
| 0000333 | Fayalite | Smyth J R, Hazen R M (1973) The crystal structures of forsterite and hortonolite at several temperatures up to 900 C American Mineralogist 58 588-593 | ![]() | 1973 | Franklin, New Jersey, USA | 0 | 573 |
| 0000572 | Fayalite | Hazen R M (1977) Effects of temperature and pressure on the crystal structure of ferromagnesian olivine American Mineralogist 62 286-295 | ![]() | 1977 | Franklin, New Jersey, USA | 0 | 873 |
| 0000334 | Fayalite | Smyth J R, Hazen R M (1973) The crystal structures of forsterite and hortonolite at several temperatures up to 900 C American Mineralogist 58 588-593 | ![]() | 1973 | Franklin, New Jersey, USA | 0 | 873 |
| 0000573 | Fayalite | Hazen R M (1977) Effects of temperature and pressure on the crystal structure of ferromagnesian olivine American Mineralogist 62 286-295 | ![]() | 1977 | Franklin, New Jersey, USA | 0 | 1173 |
| 0000335 | Fayalite | Smyth J R, Hazen R M (1973) The crystal structures of forsterite and hortonolite at several temperatures up to 900 C American Mineralogist 58 588-593 | ![]() | 1973 | Franklin, New Jersey, USA | 0 | 1173 |
| 0014999 | Fayalite | Kudoh Y, Takeda H (1986) Single crystal X-ray diffraction study on the bond compressibility of fayalite, Fe2SiO4 and rutile, TiO2 under high pressure Physica B 140 333-336 | 1986 | 0.0001 | 293 | ||
| 0000480 | Fayalite | Smyth J R (1975) High temperature crystal chemistry of fayalite olivine American Mineralogist 60 1092-1097 | ![]() | 1975 | 0 | 293 | |
| 0000174 | Fayalite | Birle J D, Gibbs G V, Moore P B, Smith J V (1968) Crystal structures of natural olivines American Mineralogist 53 807-824 | ![]() | 1968 | 0 | 293 | |
| 0000173 | Fayalite | Birle J D, Gibbs G V, Moore P B, Smith J V (1968) Crystal structures of natural olivines American Mineralogist 53 807-824 | ![]() | 1968 | 0 | 293 | |
| 0000481 | Fayalite | Smyth J R (1975) High temperature crystal chemistry of fayalite olivine American Mineralogist 60 1092-1097 | ![]() | 1975 | 0 | 573 | |
| 0000482 | Fayalite | Smyth J R (1975) High temperature crystal chemistry of fayalite olivine American Mineralogist 60 1092-1097 | ![]() | 1975 | 0 | 873 | |
| 0000483 | Fayalite | Smyth J R (1975) High temperature crystal chemistry of fayalite olivine American Mineralogist 60 1092-1097 | ![]() | 1975 | 0 | 1173 | |
| 0015000 | Fayalite | Kudoh Y, Takeda H (1986) Single crystal X-ray diffraction study on the bond compressibility of fayalite, Fe2SiO4 and rutile, TiO2 under high pressure Physica B 140 333-336 | 1986 | 4.9 | 293 | ||
| 0015001 | Fayalite | Kudoh Y, Takeda H (1986) Single crystal X-ray diffraction study on the bond compressibility of fayalite, Fe2SiO4 and rutile, TiO2 under high pressure Physica B 140 333-336 | 1986 | 6.7 | 293 | ||
| 0015002 | Fayalite | Kudoh Y, Takeda H (1986) Single crystal X-ray diffraction study on the bond compressibility of fayalite, Fe2SiO4 and rutile, TiO2 under high pressure Physica B 140 333-336 | 1986 | 9.3 | 293 | ||
| 0015003 | Fayalite | Kudoh Y, Takeda H (1986) Single crystal X-ray diffraction study on the bond compressibility of fayalite, Fe2SiO4 and rutile, TiO2 under high pressure Physica B 140 333-336 | 1986 | 11.7 | 293 | ||
| 0015004 | Fayalite | Kudoh Y, Takeda H (1986) Single crystal X-ray diffraction study on the bond compressibility of fayalite, Fe2SiO4 and rutile, TiO2 under high pressure Physica B 140 333-336 | 1986 | 14 | 293 |
CIF Raw Data - click here to close
X-Ray Powder Diffraction
Powder Diffraction Data:
| d-spacing | Intensity |
|---|---|
| 5.21 Å | (20) |
| 3.945 Å | (20) |
| 3.762 Å | (10) |
| 3.535 Å | (30) |
| 3.045 Å | (5) |
| 3.027 Å | (10) |
| 2.810 Å | (100) |
| 2.616 Å | (20) |
| 2.599 Å | (10) |
| 2.549 Å | (60) |
| 2.489 Å | (70) |
| 2.400 Å | (5) |
| 2.389 Å | (20) |
| 2.340 Å | (5) |
| 2.297 Å | (20) |
| 2.286 Å | (30) |
| 2.184 Å | (10) |
| 2.062 Å | (5) |
| 1.974 Å | (5) |
| 1.908 Å | (10) |
| 1.834 Å | (5) |
| 1.820 Å | (10) |
| 1.769 Å | (40) |
| 1.761 Å | (10) |
| 1.753 Å | (5) |
| 1.693 Å | (10) |
| 1.665 Å | (20) |
| 1.640 Å | (10) |
| 1.615 Å | (10) |
| 1.595 Å | (10) |
| 1.531 Å | (5) |
| 1.525 Å | (5) |
| 1.515 Å | (20) |
| 1.504 Å | (20) |
| 1.419 Å | (5) |
| 1.414 Å | (5) |
| 1.403 Å | (5) |
| 1.367 Å | (10) |
| 1.333 Å | (10) |
| 1.275 Å | (5) |
Comments:
ICDD 31-633 magnesian fayalite; replaces ICDD 7-158, see also ICDD 12-220 manganoan fayalite; ICDD 34-178 fayalite (synthetic)
Geological Environment
Paragenetic Mode(s):
| Paragenetic Mode | Earliest Age (Ga) |
|---|---|
| Stage 2: Planetesimal differentiation and alteration | 4.566-4.550 |
| 6 : Secondary asteroid phases | 4.566-4.560 |
| Stage 4a: Earth’s earliest continental crust | >4.4-3.0 |
| 19 : Granitic intrusive rocks | |
| Near-surface Processes | |
| 23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47) | |
| Stage 4b: Highly evolved igneous rocks | >3.0 |
| 34 : Complex granite pegmatites | |
| Stage 5: Initiation of plate tectonics | <3.5-2.5 |
| 40 : Regional metamorphism (greenschist, amphibolite, granulite facies) | |
| Stage 10b: Anthropogenic minerals | <10 Ka |
| 57 : Other minerals formed by human processes |
Type Occurrence of Fayalite
Synonyms of Fayalite
Other Language Names for Fayalite
Varieties of Fayalite
| Ferrohortonolite | Variety of fayalite, Olivine group. An intermediate member of the forsterite-fayalite series with Fe/(Fe+Mg) from 70% to 90% . |
| Roepperite (of Brush) | A manganoan, zincian fayalite. Black slightly rounded to very rounded crystals, also black cleavages. |
Relationship of Fayalite to other Species
Member of:
Other Members of Olivine Group:
| Calcio-olivine | Ca2SiO4 | Orth. mmm(2/m2/m2/m) |
| Forsterite | Mg2(SiO4) | Orth. mmm(2/m2/m2/m) |
| Glaucochroite | CaMn2+(SiO4) | Orth. mmm(2/m2/m2/m) |
| Hinokageite | MnMg(SiO4) | Orth. mm2 |
| Kirschsteinite | CaFe2+(SiO4) | Orth. mmm(2/m2/m2/m) : Pnma |
| Laihunite | (Fe3+,Fe2+,◻)2(SiO4) | Mon. 2/m : P21/b |
| Liebenbergite | Ni2(SiO4) | Orth. mmm(2/m2/m2/m) |
| Monticellite | CaMg(SiO4) | Orth. mmm(2/m2/m2/m) |
| Tephroite | Mn2+2(SiO4) | Orth. mmm(2/m2/m2/m) : Pnma |
Forms a series with:
Common Associates
Associations Based on Photo Data:
| 85 photos of Fayalite associated with Tridymite | SiO2 |
| 66 photos of Fayalite associated with Hematite | Fe2O3 |
| 55 photos of Fayalite associated with Cristobalite | SiO2 |
| 21 photos of Fayalite associated with Quartz | SiO2 |
| 20 photos of Fayalite associated with 'Obsidian' | |
| 16 photos of Fayalite associated with Grunerite | ◻Fe2+2Fe2+5(Si8O22)(OH)2 |
| 15 photos of Fayalite associated with Phlogopite | KMg3(AlSi3O10)(OH)2 |
| 11 photos of Fayalite associated with Magnetite | Fe2+Fe3+2O4 |
| 10 photos of Fayalite associated with Laihunite | (Fe3+,Fe2+,◻)2(SiO4) |
| 10 photos of Fayalite associated with Mica Group |
Related Minerals - Strunz-mindat Grouping
| 9.AC. | Poirierite | Mg2SiO4 |
| 9.AC. | Ahrensite | SiFe2O4 |
| 9.AC.05 | Laihunite | (Fe3+,Fe2+,◻)2(SiO4) |
| 9.AC.05 | Forsterite | Mg2(SiO4) |
| 9.AC.05 | Tephroite | Mn2+2(SiO4) |
| 9.AC.05 | Hinokageite | MnMg(SiO4) |
| 9.AC.05 | Liebenbergite | Ni2(SiO4) |
| 9.AC.05 | Kirschsteinite | CaFe2+(SiO4) |
| 9.AC.05 | Glaucochroite | CaMn2+(SiO4) |
| 9.AC.10 | Monticellite | CaMg(SiO4) |
| 9.AC.15 | Brunogeierite | Ge4+Fe2+2O4 |
| 9.AC.15 | Ringwoodite | (Mg,Fe2+)2SiO4 |
| 9.AC.20 | Chesnokovite | Na2[SiO2(OH)2] · 8H2O |
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.
Fayalite in petrology
An essential component of rock names highlighted in red, an accessory component in rock names highlighted in green.
Internet Links for Fayalite
mindat.org URL:
https://www.mindat.org/min-1458.html
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References for Fayalite
Reference List:
Gorgeu, Alex. (1884) Sur la production artificielle de la Fayalite. Bulletin de Minéralogie, 7 (2) 61-62 doi:10.3406/bulmi.1884.1855
Burns, Roger G., Huggins, Frank E. (1972) Cation determinative curves for Mg-Fe-Mn olivines from vibrational spectra. American Mineralogist, 57 (5-6) 967-985
Smyth, Joseph R. (1975) High temperature crystal chemistry of fayalite. American Mineralogist, 60 (11-12) 1092-1097
Hazen, Robert M. (1977) Effects of temperature and pressure on the crystal structure of ferromagnesian olivine. American Mineralogist, 62 (3-4) 286-295
Hazen, Robert M. (1977) Effects of temperature and pressure on the crystal structure of ferromagnesian olivine. American Mineralogist, 62 (3-4) 286-295
Riekel, Ch., Weiss, Armin (1978) Cation-Ordering in Synthetic Mg2-xFexSiO4-Olivines. Zeitschrift für Naturforschung B, 33. 731-736 doi:10.1515/znb-1978-0709
Fujino, K., Sasaki, S., Takéuchi, Y., Sadanaga, R. (1981) X-ray determination of electron distributions in forsterite, fayalite and tephroite. Acta Crystallographica Section B Structural Crystallography and Crystal Chemistry, 37 (3) 513-518 doi:10.1107/s0567740881003506
Suzuki, Isao, Seya, Kiyoshi, Takei, Humihiko, Sumino, Yoshio (1981) Thermal expansion of fayalite, Fe2SiO4. Physics and Chemistry of Minerals, 7 (2) 60-63 doi:10.1007/bf00309452
Mukhopadhyay, Dilip K.; Lindsley, Donald H. (1983) Phase relations in the join kirschsteinite (CaFeSiO4)-fayalite (Fe2SiO4). American Mineralogist, 68 (11-12). 1089-1094
Amthauer, G., Fuess, H., Hafner, S. S., Lottermoser, W. (1984) The magnetic structure of fayalite from 57Fe Mössbauer resonance. Acta Crystallographica Section A Foundations of Crystallography, 40 (a1). C259 doi:10.1107/s0108767384092242
Brinkmann, U., Laqua, W. (1985) Decomposition of fayalite (Fe2SiO4) in an oxygen potential gradient at 1,418 K. Physics and Chemistry of Minerals, 12 (5) 283-290 doi:10.1007/bf00310341
O'Neill, Hugh St. C. (1987) Quartz-fayalite-iron and quartz-fayalite-magnetite equilibria and the free energy of formation of fayalite (Fe2SiO4) and magnetite (Fe3O4). American Mineralogist, 72 (1-2). 67-75
Janeczek, J. (1989) Manganoan fayalite and products of its alteration from the Strzegom pegmatites, Poland. Mineralogical Magazine, 53 (371) 315-325 doi:10.1180/minmag.1989.053.371.07
Chopelas, A. (1991) Single crystal Raman spectra of forsterite, fayalite, and monticellite. American Mineralogist, 76 (7-8) 1101-1109
Mackwell, StephenJ. (1992) Oxidation kinetics of fayalite (Fe2SiO4). Physics and Chemistry of Minerals, 19 (4). 220-228 doi:10.1007/bf00202311
Pilati, T., Demartin, F., Gramaccioli, C. M. (1995) Thermal parameters for minerals of the olivine group: their implication on vibrational spectra, thermodynamic functions and transferable force fields. Acta Crystallographica Section B Structural Science, 51 (5) 721-733 doi:10.1107/s0108768194014382
Lottermoser, W., Forcher, K., Amthauer, G., Fuess, H. (1995) Powder- and single crystal Mössbauer spectroscopy on synthetic fayalite. Physics and Chemistry of Minerals, 22 (4). 259-267 doi:10.1007/bf00202259
Lottermoser, W., Forcher, K., Amthauer, G., Treutmann, W., Hosoya, S. (1996) Single crystal Mössbauer spectroscopy on the three principal sections of a synthetic fayalite sample in the antiferromagnetic state. Physics and Chemistry of Minerals, 23 (7). 432-438 doi:10.1007/bf00202029
Niemeier, D.; Chakraborty, S.; Becker, K.D. (1996) A high-temperature Mössbauer study of the directional geometry of diffusion in fayalite, Fe2SiO4. Physics and Chemistry of Minerals, 23 (4). 284 doi:10.1007/bf00207769
Redfern, S. A. T., Knight, K. S., Henderson, C. M. B., Wood, B. J. (1998) Fe-Mn cation ordering in fayalite–tephroite (FexMn1−x)2SiO4 olivines: a neutron diffraction study. Mineralogical Magazine, 62 (5) 607-615 doi:10.1180/002646198548007
Ullrich, Kerstin, Becker, Klaus Dieter (2001) Kinetics and diffusion of defects in fayalite, Fe2SiO4. Solid State Ionics, 141. 307-312 doi:10.1016/s0167-2738(01)00796-2
Kolesov, B. A.; Geiger, C. A. (2004) A Raman spectroscopic study of Fe-Mg olivines. Physics and Chemistry of Minerals, 31 (3). 142-154 doi:10.1007/s00269-003-0370-y
Kolesov, B. A., Geiger, C. A. (2004) A temperature-dependent single-crystal Raman spectroscopic study of fayalite: evidence for phonon-magnetic excitation coupling. Physics and Chemistry of Minerals, 31 (3) 155-161 doi:10.1007/s00269-003-0369-4
Localities for Fayalite
Showing 610 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.
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The
Caspar quarry, Ettringen, Vordereifel, Mayen-Koblenz, Rhineland-Palatinate, Germany