PRESSURE-VOLUME-TEMPERATURE EQUATION OF STATE OF ANDRADITE AND GROSSULAR, BY HIGH-PRESSURE AND -TEMPERATURE POWDER DIFFRACTION
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dc.contributor.author | Pavese A. | |
dc.contributor.author | Diella V. | |
dc.contributor.author | Pischedda V. | |
dc.contributor.author | Merli M. | |
dc.contributor.author | Bocchio R. | |
dc.contributor.author | Mezouar M. | |
dc.date.accessioned | 2021-03-30T10:40:29Z | |
dc.date.available | 2021-03-30T10:40:29Z | |
dc.date.issued | 2001 | |
dc.identifier | https://www.elibrary.ru/item.asp?id=872472 | |
dc.identifier.citation | Physics and Chemistry of Minerals, 2001, 28, 4, 242-248 | |
dc.identifier.issn | 0342-1791 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/27187 | |
dc.description.abstract | The thermoelastic parameters of natural andradite and grossular have been investigated by high-pressure and -temperature synchrotron X-ray powder diffraction, at ESRF, on the ID30 beamline. The P–V–T data have been fitted by Birch-Murnaghan-like EOSs, using both the approximated and the general form. We have obtained for andradite K 0=158.0(±1.5) GPa, (dK/dT )0=−0.020(3) GPa K−1 and α0=31.6(2) 10−6 K−1, and for grossular K 0=168.2(±1.7) GPa, (dK/dT)0=−0.016(3) GPa K−1 and α0=27.8(2) 10−6 K−1. Comparisons between the present issues and thermoelastic properties of garnets earlier determined are carried out. | |
dc.subject | ANDRADITE | |
dc.subject | GROSSULAR | |
dc.subject | T EOS | |
dc.subject | X-RAY POWDER DIFFRACTION | |
dc.title | PRESSURE-VOLUME-TEMPERATURE EQUATION OF STATE OF ANDRADITE AND GROSSULAR, BY HIGH-PRESSURE AND -TEMPERATURE POWDER DIFFRACTION | |
dc.type | Статья |
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