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IMA database
Reference A
Blomstrand C W
(1868)
Om Westanå mineralier. Öfversigt af Kongliga Vetenskaps-Akademiens Förhandlingar
25,
197-212
[view file]
Reference B
Onac B P, Effenberger H S
(2007)
Re-examination of berlinite (AlPO4) from the Cioclovina Cave, Romania. American Mineralogist
92,
1998-2001
[view file]
References
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25,
197-212
[view file]
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(1998)
Structural properties of α-berlinite (AlPO4). Physics and Chemistry of Minerals
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(2003)
Modeling the framework stability and catalytic activity of pure and transition metal - doped zeotypes. Journal of Solid State Chemistry
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Raman study of AlPO4 (berlinite) at the α–β transition. Journal of Physics: Condensed Matter
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Crystal chemistry of schoonerite-group minerals. European Journal of Mineralogy
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Secondary Zn-bearing phosphate minerals associated with alteration of phosphophyllite at Hagendorf-Süd, Bavaria. European Journal of Mineralogy
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Huttenlocher H F
(1935)
Kristallstruktur des Aluminiumorthophosphates AlPO4. Zeitschrift für Kristallographie
90,
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Jayaraman A, Wood D L, Maines R G
(1987)
High-pressure Raman study of the vibrational modes in AlPO4 and SiO2 (α-quartz). Physical Review B
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Marincea S, Dumitras D G
(2005)
First reported sedimentary occurrence of berlinite (AlPO4) in phosphate-bearing sediments from Cioclovina Cave, Romania—comment. American Mineralogist
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(1997)
The temperature dependence of the crystal structure of berlinite, a quartz-type form of AlPO4. Physics and Chemistry of Minerals
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[view file]
Onac B P, Effenberger H S
(2007)
Re-examination of berlinite (AlPO4) from the Cioclovina Cave, Romania. American Mineralogist
92,
1998-2001
[view file]
Onac B P, White W B
(2003)
First reported sedimentary occurrence of berlinite (AlPO4) in phosphate-bearing. American Mineralogist
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(2000)
Anharmonicity of zone-centre optical phonons: Raman spectra of the isomorphous α-quartz, berlinite and gallium phosphate in the temperature range 8–300 K. Journal of Raman Spectroscopy
31,
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Scott J F
(1971)
Raman spectra and lattice dynamics of α-berlinite (AlPO4). Physical Review B
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