High-pressure behaviour along the jadeite NaAlSi2O6-aegirine NaFeSi2O6 solid solution up to 10 GPa

被引:51
|
作者
Nestola, Fabrizio
Ballaran, Tiziana Boffa
Liebske, Christian
Bruno, Marco
Tribaudino, Mario
机构
[1] Univ Bayreuth, Bayer Geoinst, D-95447 Bayreuth, Germany
[2] Virginia Tech, Crystallog Lab, Dept Geosci, Blacksburg, VA 24061 USA
[3] Univ Turin, Dipartimento Sci Mineral & Petrol, I-10125 Turin, Italy
[4] Univ Parma, Dipartimento Sci Terra, I-43100 Parma, Italy
关键词
high-pressure; Na-pyroxenes; single-crystal; X-ray diffraction; compressibility;
D O I
10.1007/s00269-006-0089-7
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
The volume variation as a function of pressure along the jadeite-aegirine solid solution was determined at room temperature up to pressures between 6.5 and 9.7 GPa by single-crystal X-ray diffraction. The unit-cell volumes collected at room pressure for the different compositions indicate a slight deviation from linearity along the join. The pressure-volume data have been fitted using a third-order Birch-Murnaghan equation of state (BM3-EoS). The bulk modulus, K (T0), varies from 134.0(7) GPa for pure jadeite to 116.1(5) GPa for pure aegirine. Its evolution with composition along the join is not linear and can be described by the following second order polynomial: K-T0 = 116.2(5) + [0.25(3) x (mol%Jd)] -[0.0008(3) x (mol%Jd)(2)] The value of the first pressure derivative K' is close to 4 for all the samples investigated and can be used in a BM3-EoS to determine the volume variations of these pyroxenes up to 7-10 GPa. Along the join the highest compressibility among the crystallographic directions is always observed along a, however, the compression along b is the most affected by compositional changes. The strain ellipsoid analysis indicates that the major compression occurs on the (0 1 0) plane along a direction at about 145 degrees to the c axis (from c to a). The anisotropy of the compression increases with increasing the aegirine component, as confirmed by the analysis of both the axial compressibility and the strain tensor.
引用
收藏
页码:417 / 425
页数:9
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