The high-pressure and temperature equation of state of a majorite solid solution in the system of Mg4Si4O12-Mg3Al2Si3O12

被引:28
作者
Morishima, H
Ohtani, E [1 ]
Kato, T
Kubo, T
Suzuki, A
Kikegawa, T
Shimomura, O
机构
[1] Tohoku Univ, Inst Mineral Petrol & Econ Geol, Sendai, Miyagi, Japan
[2] Natl Lab High Energy Phys, Photon Factory, Tsukuba, Ibaraki, Japan
关键词
majorite garnet; X-ray diffraction; PVT observation;
D O I
10.1007/s002690050234
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
The high-pressure and temperature equation of state of majorite solid solution, Mj(0.8)Py(0.2), was determined up to 23 GPa and 773 K with energy-dispersive synchrotron X-ray diffraction at high pressure and high temperature using the single- and double-stage configurations of the multianvil apparatuses, MAX80 and 90, The X-ray diffraction data of the majorite sample were analyzed using the WPPD (whole-powder-pattern de-composition) method to obtain the lattice parameters. A least-squares fitting using the third-order Birch-Murnaghan equation of state yields the isothermal bulk modulus, K-T0 = 156 GPa, its pressure derivative, K' = 4.4(+/- 0.3), and temperature derivative (partial derivative K-T/ partial derivative T)(p) = -1.9(+/- 0.3)x 10(-2) GPa/K, assuming that the thermal expansion coefficient is similar to that of pyrope-almandine solid solution.
引用
收藏
页码:3 / 10
页数:8
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