1959
DOI: 10.1524/zkri.1959.111.1-6.451
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High-pressure region of the silica isotypes

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Cited by 81 publications
(17 citation statements)
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“…A study of the effect of temperature on natural stishovite was also made a-f3 quartz boundary by Yoder (1950). Quartz-Coesite boundary (lower temperature) by Dachille and Roy (1959a) and the other by Boyd and England (1960). Coesite-stishovite boundary (lower temperature) by Ostrovsky (1966) and the other by Stishov and Popova (1963).…”
Section: Introductionmentioning
confidence: 99%
“…A study of the effect of temperature on natural stishovite was also made a-f3 quartz boundary by Yoder (1950). Quartz-Coesite boundary (lower temperature) by Dachille and Roy (1959a) and the other by Boyd and England (1960). Coesite-stishovite boundary (lower temperature) by Ostrovsky (1966) and the other by Stishov and Popova (1963).…”
Section: Introductionmentioning
confidence: 99%
“…Gerrard and Griffey (4) discussed a novel preparation of boron phosphate from triethyl phosphate and boron trichloride. A number of papers (5,6,7) have been concerned with high-pressure forms of boron phosphate. V. F. Ross and co-workers (8) prepared boron phosphate for their n.m.r.…”
Section: Introductionmentioning
confidence: 99%
“…The ratio for the A1AS0 4 polymorphs is 1.51 and the ratio for the Si0 2 polymorphs is 1.49 (SCLAR et al, 1962). The mean of the three published values for the GeO a polymorphs, which range from 1.48 to 1.54, is 1.51 (LIPPIN- COTT et al, 1958;DACHILLE andROY, 1959, andSCLAR et al, 1962). The effect of coordination on the force constant, therefore, is apparently independent of the chemical composition.…”
Section: Fig 2 Infra-red Absorption Spectra Of the Quartz And Rutilmentioning
confidence: 93%
“…Rutile structure was dominant at about 0.40. DACHILLE and ROY (1959A) suggested that some AB0 4 compounds, not normally rutile, with radius ratios close to 0.40 might be converted to the rutile structure at high pressure. The recent conversion of Si0 2 to the rutile structure at about 120 kbar and 1200C (STISHOV and BELOV, 1962) furnished some experimental basis for the possibility that some AB0 4 compounds, which normally have the quartz structure, might also be converted to the rutile structure at sufficiently high pressure and temperature.…”
Section: Introductionmentioning
confidence: 99%