Physics and Chemistry of Minerals

, Volume 15, Issue 4, pp 313–318 | Cite as

Comparative compressibility of end-member feldspars

  • R. J. Angel
  • R. M. Hazen
  • T. C. McCormick
  • C. T. Prewitt
  • J. R. Smyth
Article

Abstract

The compressibilities of the three end-member feldspars have been determined between 1 bar and 50 kbar by single crystal X-ray diffraction techniques, using a Merrill-Bassett type diamond anvil cell with three crystals loaded simultaneously. Low albite (ordered aluminium-silicon distribution) and high sanidine (disordered Al-Si) show similar behaviour on compression, with bulk moduli (linear fit to volume-pressure data) of 0.70 and 0.67 Mbar respectively. The most compressible cell axis of all three feldspars studied is a, indicating that the major change in the feldspar framework with pressure is a shortening of the overall length of the “crankshaft chains” by reduction of T-O-T angles.

Anorthite shows anomalous behaviour in that we have observed a previously unreported reversible phase transition at a pressure between 25.5 and 29.5 kbar. This transition is marked by large discontinuities in the unit cell angles and a small decrease of 0.2 percent in the cell volume with increasing pressure. The high-pressure phase is less compressible than the low-pressure phase, the bulk moduli being 0.94 and 1.06 Mbar respectively. There was no evidence of a monoclinic to triclinic inversion in sanidine that was expected to occur between 20 and 30 kbar on the basis of previous work on intermediate alkali feldspars.

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Copyright information

© Springer-Verlag 1988

Authors and Affiliations

  • R. J. Angel
    • 1
  • R. M. Hazen
    • 1
  • T. C. McCormick
    • 2
  • C. T. Prewitt
    • 1
  • J. R. Smyth
    • 2
  1. 1.Geophysical LaboratoryCarnegie Institution of WashingtonWashington DCUSA
  2. 2.Department of Geological SciencesUniversity of ColoradoBoulderUSA

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