Determination of elastic constants of single-crystal chromian spinel by resonant ultrasound spectroscopy and implications for fluid inclusion geobarometry

We determined elastic constants of a single-crystal chromian spinel at temperatures from −15 to 45 °C through the Rectangular Parallelepiped Resonance method. The sample is a natural chromian spinel, which was separated from a mantle xenolith. Elastic constants at an ambient temperature ( T  = 24.0 ...

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Veröffentlicht in:Physics and chemistry of minerals 2018-03, Vol.45 (3), p.237-247
Hauptverfasser: Ono, Kenya, Harada, Yuya, Yoneda, Akira, Yamamoto, Junji, Yoshiasa, Akira, Sugiyama, Kazumasa, Arima, Hiroshi, Watanabe, Tohru
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container_end_page 247
container_issue 3
container_start_page 237
container_title Physics and chemistry of minerals
container_volume 45
creator Ono, Kenya
Harada, Yuya
Yoneda, Akira
Yamamoto, Junji
Yoshiasa, Akira
Sugiyama, Kazumasa
Arima, Hiroshi
Watanabe, Tohru
description We determined elastic constants of a single-crystal chromian spinel at temperatures from −15 to 45 °C through the Rectangular Parallelepiped Resonance method. The sample is a natural chromian spinel, which was separated from a mantle xenolith. Elastic constants at an ambient temperature ( T  = 24.0 °C) are C 11  = 264.8(1.7) GPa, C 12  = 154.5(1.8) GPa and C 44  = 142.6(0.3) GPa. All the elastic constants decrease linearly with increasing temperature. The temperature derivatives are d C 11 /d T  = −0.049(2) GPa/°K, d C 12 /d T  = −0.019(1) GPa/°K and d C 44 /d T  = −0.020(1) GPa/°K. As an implication of the elastic constants, we applied them to the correction of a fluid inclusion geobarometry, which utilizes residual pressure of fluid inclusion as a depth scale. Before entrainment by a magma, the fluid inclusions must have the identical fluid density in constituent minerals of a xenolith. It has been, however, pointed out that fluid density of fluid inclusions significantly varies with host mineral species. The present study elucidates that elastic constants and thermal expansion coefficients cannot explain the difference in fluid density among mineral species. The density difference would reflect the difference in the degree of plastic deformation in the minerals.
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The sample is a natural chromian spinel, which was separated from a mantle xenolith. Elastic constants at an ambient temperature ( T  = 24.0 °C) are C 11  = 264.8(1.7) GPa, C 12  = 154.5(1.8) GPa and C 44  = 142.6(0.3) GPa. All the elastic constants decrease linearly with increasing temperature. The temperature derivatives are d C 11 /d T  = −0.049(2) GPa/°K, d C 12 /d T  = −0.019(1) GPa/°K and d C 44 /d T  = −0.020(1) GPa/°K. As an implication of the elastic constants, we applied them to the correction of a fluid inclusion geobarometry, which utilizes residual pressure of fluid inclusion as a depth scale. Before entrainment by a magma, the fluid inclusions must have the identical fluid density in constituent minerals of a xenolith. It has been, however, pointed out that fluid density of fluid inclusions significantly varies with host mineral species. The present study elucidates that elastic constants and thermal expansion coefficients cannot explain the difference in fluid density among mineral species. 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The present study elucidates that elastic constants and thermal expansion coefficients cannot explain the difference in fluid density among mineral species. 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The sample is a natural chromian spinel, which was separated from a mantle xenolith. Elastic constants at an ambient temperature ( T  = 24.0 °C) are C 11  = 264.8(1.7) GPa, C 12  = 154.5(1.8) GPa and C 44  = 142.6(0.3) GPa. All the elastic constants decrease linearly with increasing temperature. The temperature derivatives are d C 11 /d T  = −0.049(2) GPa/°K, d C 12 /d T  = −0.019(1) GPa/°K and d C 44 /d T  = −0.020(1) GPa/°K. As an implication of the elastic constants, we applied them to the correction of a fluid inclusion geobarometry, which utilizes residual pressure of fluid inclusion as a depth scale. Before entrainment by a magma, the fluid inclusions must have the identical fluid density in constituent minerals of a xenolith. It has been, however, pointed out that fluid density of fluid inclusions significantly varies with host mineral species. The present study elucidates that elastic constants and thermal expansion coefficients cannot explain the difference in fluid density among mineral species. The density difference would reflect the difference in the degree of plastic deformation in the minerals.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.1007/s00269-017-0912-3</doi><tpages>11</tpages></addata></record>
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subjects Ambient temperature
Crystallography and Scattering Methods
Crystals
Deformation mechanisms
Density
Earth and Environmental Science
Earth Sciences
Elastic properties
Entrainment
Fluid inclusions
Geochemistry
Magma
Magnetism
Mineral Resources
Mineralogy
Minerals
Original Paper
Parallelepipeds
Plastic deformation
Single crystals
Spinel
Thermal expansion
title Determination of elastic constants of single-crystal chromian spinel by resonant ultrasound spectroscopy and implications for fluid inclusion geobarometry
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