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Behavior of rock salt, limestone, and anhydrite during indentation
Indentation and compression are compared; deformation of rock salt is predominantly due to gliding; both single grains and rock work hardened just under indenter; deformation of other rocks was due to combination of gliding and microfracturing; approximate stress and strain fields were found for deformed zone, from which average values of stress difference, confining pressure, and strain could be determined.
Behavior of rock salt, limestone, and anhydrite during indentation
Indentation and compression are compared; deformation of rock salt is predominantly due to gliding; both single grains and rock work hardened just under indenter; deformation of other rocks was due to combination of gliding and microfracturing; approximate stress and strain fields were found for deformed zone, from which average values of stress difference, confining pressure, and strain could be determined.
Behavior of rock salt, limestone, and anhydrite during indentation
J Geophysical Research
Brace, W.F. (author)
1960
16 pages
Article (Journal)
English
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