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Shock wave equation of state of muscoviteShock wave data were obtained between 20 and 140 GPa for natural muscovite obtained from Methuen Township (Ontario), in order to provide a shock-wave equation of state for this crustal hydrous mineral. The shock equation of state data could be fit by a linear shock velocity (Us) versus particle velocity (Up) relation Us = 4.62 + 1.27 Up (km/s). Third-order Birch-Murnaghan equation of state parameters were found to be K(OS) = 52 +/-4 GPa and K-prime(OS) = 3.2 +/-0.3 GPa. These parameters are comparable to those of other hydrous minerals such as brucite, serpentine, and tremolite.
Document ID
19920032044
Acquisition Source
Legacy CDMS
Document Type
Reprint (Version printed in journal)
Authors
Sekine, Toshimori
(California Inst. of Tech. Pasadena, CA, United States)
Rubin, Allan M.
(California Inst. of Tech. Pasadena, CA, United States)
Ahrens, Thomas J.
(California Institute of Technology Pasadena, United States)
Date Acquired
August 15, 2013
Publication Date
November 10, 1991
Publication Information
Publication: Journal of Geophysical Research
Volume: 96
ISSN: 0148-0227
Subject Category
Geophysics
Accession Number
92A14668
Funding Number(s)
CONTRACT_GRANT: F19628-88-K-0034
Distribution Limits
Public
Copyright
Other

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