Forsterite R040052

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Record 3053 of 4216  

Name: Forsterite
RRUFF ID: R040052
Ideal Chemistry: Mg2(SiO4)
Locality: Synthetic, Czochralski method
Source: Hideki Kanazawa of Kyoto University, Japan
Owner: RRUFF
Description: Colorless crystal fragments obtained from a boule.
Status: The identification of this mineral has been confirmed by X-ray diffraction and chemical analysis
Mineral Group: [ Olivine (61) ]
Quick search: [ All Forsterite samples (20) ]
CHEMISTRY 
RRUFF ID: R040052.2
Sample Description: Microprobe Fragment
Measured Chemistry: Mg2.00Si1.00O4
Microprobe Data File: [ Download Excel File ]
RAMAN SPECTRUM 
RRUFF ID:
Sample Description: Sample is oriented, mounted onto a pin and polished
Pin ID: l00104
Orientation: Laser parallel to  -a*  (-1 0 0).     Fiducial mark perpendicular to laser is parallel to  b   [0 1 0].
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Raman Mode Analysis
Direction of polarization of laser relative to fiducial mark:
X Min:    X Max:    X Sort:
BROAD SCAN WITH SPECTRAL ARTIFACTS
RRUFF ID: R040052
Wavelength:
Sample Description: Unoriented sample
Instrument settings: Thermo Almega XR 532nm @ 100% of 150mW
INFRARED SPECTRUM (Attenuated Total Reflectance) 
RRUFF ID: R040052.1
Instrument settings: SensIR Durascope on a Nicolet Magna 860 FTIR
Resolution:
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POWDER DIFFRACTION 
RRUFF ID: R040052.1
Sample Description: Powder
Cell Refinement Output: a: 4.7558(2)Å    b: 10.1965(4)Å    c: 5.9817(2)Å
alpha: 90.°    beta: 90.°    gamma: 90.°   Volume: 290.07(1)Å3    Crystal System: orthorhombic
  File Type Information Close
Calculated diffraction file.

  File Type Information Close
Output file from the Bruker D8 Advance instrument. Includes device headers and XY data.

  File Type Information Close
Output file from the Bruker D8 Advance instrument. Includes device headers and XY data.

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REFERENCES for Forsterite

American Mineralogist Crystal Structure Database Record: [view record]

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Nover G, Will G (1981) Structure refinements of seven natural olivine crystals and the influence of the oxygen partial pressure on the cation distribution, Zeitschrift für Kristallographie, 155, 27-45   [view file]

Nord A G, Annersten H, Filippidis A (1982) The cation distribution in synthetic Mg-Fe-Ni olivines, American Mineralogist, 67, 1206-1211   [view file]

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Kroll H, Kirfel A, Heinemann R (2014) Axial thermal expansion and related thermophysical parameters in the Mg,Fe olivine solid-solution series, European Journal of Mineralogy, 26, 607-621

Ejima T, Akasaka M, Nagao T, Ohfuji H (2015) Occurrence of Fe3+ and formation process of precipitates within oxidized olivine phenocrysts in basalt lava from Kuroshima volcano, Goto islands, Nagasaki, Japan, Mineralogical Magazine, 79, 1833-1848

Yang Y, Wang Z, Smyth J R, Liu J, Xia Q (2015) Water effects on the anharmonic properties of forsterite, American Mineralogist, 100, 2185-2190

Azevedo S, Nespolo M (2016) Twinning in olivine group revisited, European Journal of Mineralogy, 29, 213-226

Balan E, Blanchard M, Lazzeri M, Ingrin J (2017) Theoretical Raman spectrum and anharmonicity of tetrahedral OH defects in hydrous forsterite, European Journal of Mineralogy, 29, 201-212

Breitenfeld L B, Dyar M D, Carey C J, Tague T J, Wang P, Mullen T, Parente M (2018) Predicting olivine composition using Raman spectroscopy through band shift and multivariate analyses, American Mineralogist, 103, 1827-1836

Morrison S M, Downs R T, Blake D F, Prabhu A, Eleish A, Vaniman D T, Ming D W, Rampe E B, Hazen R M, Achilles C N, Treiman A H, Yen A S, Morris R V, Bristow T F, Chipera S J, Sarrazin P C, Fendrich K V, Morookian J M, Farmer J D, Des Marais D J, Craig P I (2018) Relationships between unit-cell parameters and composition for rock-forming minerals on Earth, Mars, and other extraterrestrial bodies, American Mineralogist, 103, 848-856   [view file]

Morrison S M, Downs R T, Blake D F, Vaniman D T, Ming D W, Hazen R M, Treiman A H, Achilles C N, Yen A S, Morris R V, Rampe E B, Bristow T F, Chipera S J, Sarrazin P C, Gellert R, Fendrich K V, Morookian J M, Farmer J D, Des Marais D J, Craig P I (2018) Crystal chemistry of martian minerals from Bradbury Landing through Naukluft Plateau, Gale crater, Mars, American Mineralogist, 103, 857-871   [view file]

Nesbitt H W, Bancroft G M, Henderson G S (2018) Temperature dependence of Raman shifts and line widths for Q0 and Q2 crystals of silicates, phosphates, and sulphates, American Mineralogist, 103, 966-976

Knafelc J, Filiberto J, Ferré E C, Conder J A, Costello L, Crandall J R, Dyar M D, Friedman S A, Hummer D R, Schwenzer S P (2019) The effect of oxidation on the mineralogy and magnetic properties of olivine, American Mineralogist, 104, 694-702

Xu J, Fan D, Zhang D, Li B, Zhou W, Dera P K (2020) Investigation of the crystal structure of a low water content hydrous olivine to 29.9 GPa: A high-pressure single-crystal X-ray diffraction study, American Mineralogist, 105, 1857-1865

Geiger C A, Vielreicher N M, Dachs E (2021) Are the thermodynamic properties of natural and synthetic Mg2SiO4-Fe2SiO4 olivines the same?, American Mineralogist, 106, 317-321

Liu D, Guo X, Smyth J R, Wang X, Zhu X, Miao Y, Bai J, Ye Y (2021) High-temperature and high-pressure Raman spectra of Fo89Fa11 and Fo58Fa42 olivines: Iron effect on thermodynamic properties, American Mineralogist, 106, 1668-1678