1986
DOI: 10.1007/bf00311896
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High-pressure crystal chemistry of phenakite (Be2SiO4) and bertrandite (Be4Si2O7(OH)2)

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1987
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Cited by 77 publications
(51 citation statements)
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“…3). This result in this study is very consistent with those collected with X-ray diffraction method in the study of Hazen et al (1986) and Qin et al (2008), whereas it is different with the conclusions made by Prencipe et al (2011) in terms of ab initio calculation method that Prencipe et al (2011) predicted a phase transition of zone-center soft mode from P6/ mcc to P1 will occur at a pressure about 14 GPa. Furthermore, for the room-temperature and high-pressure singlecrystal X-ray diffraction data, we fitted the P-V data to the third-order BM-EoS to derive the elastic parameters of beryl.…”
Section: Resultssupporting
confidence: 57%
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“…3). This result in this study is very consistent with those collected with X-ray diffraction method in the study of Hazen et al (1986) and Qin et al (2008), whereas it is different with the conclusions made by Prencipe et al (2011) in terms of ab initio calculation method that Prencipe et al (2011) predicted a phase transition of zone-center soft mode from P6/ mcc to P1 will occur at a pressure about 14 GPa. Furthermore, for the room-temperature and high-pressure singlecrystal X-ray diffraction data, we fitted the P-V data to the third-order BM-EoS to derive the elastic parameters of beryl.…”
Section: Resultssupporting
confidence: 57%
“…Subsequently, Qin et al (2008) studied the compression behavior of beryl up to 19.2 GPa, using diamond anvil cell in conjunction with in situ synchrotron radiation energy-dispersive X-ray diffraction, and obtained the K 0 value as 226 ± 6 GPa with fixed K ′ 0 at 4. Their calculations are different from both results obtained by Hazen et al (1986) (K 0 = 170 ± 5 GPa) and by Prencipe and Nestola (2005) …”
Section: Introductioncontrasting
confidence: 75%
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