SOUND VELOCITIES AND ELASTIC PROPERTIES OF γ-MG2SIO4 TO 873 K BY BRILLOUIN SPECTROSCOPY
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dc.contributor.author | Jackson J.M. | |
dc.contributor.author | Sinogeikin S.V. | |
dc.contributor.author | Bass J.D. | |
dc.date.accessioned | 2021-01-30T12:21:15Z | |
dc.date.available | 2021-01-30T12:21:15Z | |
dc.date.issued | 2000 | |
dc.identifier | https://elibrary.ru/item.asp?id=13954020 | |
dc.identifier.citation | American Mineralogist, 2000, 85, 2, 296-303 | |
dc.identifier.issn | 0003-004X | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/24061 | |
dc.description.abstract | The sound velocities and single-crystal elastic moduli of spinel-structured γ-Mg2SiO4 were measured to 873 K by Brillouin spectroscopy using a new high-temperature cell designed for single-crystal measurements. These are the first reported acoustic measurements of γ-Mg2SiO4 elasticity at high temperatures. A linear decrease of elastic moduli and sound velocities with temperature adequately describes the data. The adiabatic bulk modulus, KS, shear modulus, μ, and respective temperature derivatives for γ-Mg2SiO4 are: KS = 185(3) GPa, μ = 120.4(2.0) GPa, (∂KS/∂T)P = −0.024(3) GPa/K and (∂μ/∂T)P = −0.015(2) GPa/K. Extrapolation of our data to transition zone pressures and temperatures indicates that the shear and compressional impedance contrasts associated with β- →γ-(Mg,Fe)2SiO4 transition are sufficient to produce an observable discontinuity at 520 km depth, even with a moderate (30–50%) amount of olivine. | |
dc.title | SOUND VELOCITIES AND ELASTIC PROPERTIES OF γ-MG2SIO4 TO 873 K BY BRILLOUIN SPECTROSCOPY | |
dc.type | Статья |
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