Dilatancy in the Fracture of Crystalline Rocks
Abstract
Volume changes of a granite, a marble, and an aplite were measured during deformation in triaxial compression at confining pressure of as much as 8 kb. Stress-volumetric strain behavior is qualitatively the same for these rocks and a wide variety of other rocks and concrete studied elsewhere. Volume changes are purely elastic at low stress. As the maximum stress becomes one-third to two-thirds the fracture stress at a given pressure, the rocks...
Paper Details
Title
Dilatancy in the Fracture of Crystalline Rocks
Published Date
Aug 15, 1966
Volume
71
Issue
16
Pages
3939 - 3953
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