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1 Bayerisches Geoinstitut, Universität Bayreuth, 95440 Bayreuth, Germany
2 Dipartimento di Scienze Mineralogiche e Petrologiche, Via Valperga Caluso 35, I-10125 Torino, Italy
3 Istituto di Geoscienze e Georisorse, CNR, Sezione di Torino, Via Accademia delle Scienze 5, I-10123 Torino, Italy
Correspondence: * E-mail: piera.benna{at}unito.ital.
A synthetic feldspar of composition Ca0.2Sr0.8Al2Si2O8 (An20SrF80) (space group I
at room condition, Qod = 0.88) was investigated using in situ high-pressure single-crystal X-ray diffraction. Unit-cell parameters were measured as a function of pressure to 7.7 GPa at room T. Two reversible phase transitions were observed in the investigated pressure range. A first-order triclinic I
to monoclinic I2/c phase transition was observed at P ~ 4.3 GPa. Several cycles through the transformation were made to constrain the hysteresis (~0.3 GPa). The discontinuous character of the transition is especially noticeable in the behavior of the
angle, which increases from 90.55° to 91.04° before Ptr. The Murnaghan EoS parameters obtained for the volume are: V0 = 1393.97(6) Å3, K0 = 88.7(5) GPa, K' = 1.3(3) for the triclinic I
phase and V0 = 1396.9(1) Å3, K0 = 89.4(9) GPa, K' = 1.7(6) for the monoclinic I2/c phase whose high-P behavior appears, therefore, linear in the pressure range of its stability. The axial compressibility scheme is ßa > ßc > ßb for both phases, in good agreement with previous observations for other feldspars. A similar displacive ferroelastic I
-I2/c phase transition was observed for the same sample with increasing temperature. At P ~ 7.3 GPa a large discontinuity in the unit-cell parameters indicates a further transition from monoclinic I2/c phase to monoclinic-II phase. This transformation is strongly fist order with a volume change of about 1.7%.
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P. Benna, F. Nestola, T. B. Ballaran, T. Balic-Zunic, L. F. Lundegaard, and E. Bruno The high-pressure structural configurations of Ca0.2Sr0.8Al2Si2O8 feldspar: The IFormula-I2/c and I2/c-P21/c phase transitions American Mineralogist, July 1, 2007; 92(7): 1190 - 1199. [Abstract] [Full Text] [PDF] |
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