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A room-temperature phase transition in maximum microcline
Authors:R. E. Openshaw  C. M. B. Henderson  W. L. Brown
Affiliation:1. Centre de Recherches Pétrographiques et Géochimiques, C.O. No. 1, F-54500, Vandoeuvre-les-Nancy, France
2. U.S. Geological Survey, 22092, Reston, Virginia, U.S.A.
Abstract:A type of hysteresis, similar to that observed in the heat capacity measurements (Openshaw et al., 1979), has been found in the room temperature unit cell parameters of a microcline sample 71104 and likewise indicates the existence of two forms of this microcline. The A-form (obtained on cooling the sample to approximately 80 K) has significantly different values of b, β and V to the B-form which is the more stable form above 300±10 K. The transition from the A- to the B-form occurs over a period of months and has an associated ΔV of ?0.0011 nm3. The cell parameters of the B-form have been measured up to 1278 K and show significant changes: a and V increase, b constracts, and c is unchanged on increasing temperature. The calculated thermal expansion ellipsoid is nearly uniaxial and similar in shape to that for sanidine. Below room temperature the isobaric thermal expansion coefficent αp, for a natural microcline is nearly four times as large as that for sanidine. Above room temperature αp for 71104 microcline decreases markedly with increasing temperature. This implies a rapid change in the thermal expansion behavior of microcline which has been correlated with the proposed phase transition.
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