Thermal expansion along the NaAlSi2O6–NaFe3+Si2O6 and NaAlSi2O6–CaFe2+Si2O6 solid solutions

被引:1
|
作者
Mario Tribaudino
Fabrizio Nestola
Marco Bruno
Tiziana Boffa Ballaran
Christian Liebske
机构
[1] Università di Parma,Dipartimento di Scienze della Terra
[2] Università di Padova,Dipartimento di Geoscienze
[3] Università di Torino,Dipartimento di Scienze Mineralogiche e Petrologiche
[4] Universität Bayreuth,Bayerisches Geoinstitut
[5] ETH Zurich,Institute for Mineralogy and Petrology
[6] Corus RD&T,undefined
[7] Ceramics Research Centre,undefined
来源
Physics and Chemistry of Minerals | 2008年 / 35卷
关键词
Single-crystal; X-ray diffraction; High-temperature; Clinopyroxene;
D O I
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学科分类号
摘要
The high temperature volume and axial parameters for six C2/c clinopyroxenes along the NaAlSi2O6–NaFe3+Si2O6 and NaAlSi2O6–CaFe2+Si2O6 joins were determined from room T up to 800°C, using integrated diffraction profiles from in situ high temperature single crystal data collections. The thermal expansion coefficient was determined by fitting the experimental data according to the relation: ln(V/V0) = α(T − T0). The thermal expansion coefficient increases by about 15% along the jadeite–hedenbergite join, whereas it is almost constant between jadeite and aegirine. The increase is related to the Ca for Na substitution into the M2 site; the same behaviour was observed along the jadeite–diopside solid solution, which presents the same substitution at the M2 site. Strain tensor analysis shows that the major deformation with temperature occurs in all samples along the b axis; on the (010) plane the higher deformation occurs in jadeite and aegirine at a direction almost normal to the tetrahedral–octahedral planes, and in hedenbergite along the projection of the longer M2–O bonds. The orientation of the strain ellipsoid with temperature in hedenbergite is close to that observed with pressure in pyroxenes. Along the jadeite–aegirine join instead the high-temperature and high-pressure strain are differently oriented.
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页码:241 / 248
页数:7
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