EFFECT OF STRAIN RATE ON THE DEFORMATIONAL BEHAVIOR OF ROCK.
Abstract
Experimental results for four different rock types in which the microscopic mechanisms of deformation vary in their contribution to the total deformation indicate that cataclastic deformation is independent of time. It appears that the physical behavior of materials deforming cataclastically can thus be evaluated in terms of pressure and temperature alone. The magnitude of previous strain affects the elastic moduli, ductility, and strength of a rock subjected to later deformation, but the effect depends largely on the conditions of the later deformation--in particular, on the confining pressure and orientation of the principal stresses. (Author)
Document Details
- Document Type
- Technical Report
- Publication Date
- Dec 30, 1968
- Accession Number
- AD0681939
Entities
People
- Fred A. Donath
Organizations
- Columbia University