Contrasting dilatant behaviors of mafic and ultramafic rocks based on triaxial deformation experiments
Author:
Affiliation:
1. Department of Earth and Planetary Systems Science, Hiroshima University
Publisher
Japan Association of Mineralogical Sciences
Subject
Geology,Geophysics
Link
https://www.jstage.jst.go.jp/article/jmps/114/2/114_181120/_pdf
Reference28 articles.
1. Brace, W.F. and Bombolakis, E.G. (1963) A Note on Brittle Crack Growth in Compression. Journal of Geophysical Research, 68, 3709–3713.
2. Brace, W.F., Paulding, B.W. and Scholz, C. (1966) Dilatancy in the fracture of crystalline rocks. Journal of Geophysical Research, 71, 3939–3953.
3. Cotterell, B. and Rice, J.R. (1980) Slightly curved or kinked cracks. International Journal of Fracture, 16, 155–169.
4. David, E.C., Brantut, N., Hansen, L.N. and Mitchell, T.M. (2018) Absence of Stress–induced Anisotropy during Brittle Deformation in Antigorite Serpentinite. Journal of Geophysical Research: Solid Earth, 123.
5. Escartín, J., Hirth, G. and Evans, B. (1997) Nondilatant brittle deformation of serpentinites: Implications for Mohr–Coulomb theory and the strength of faults. Journal of Geophysical Research, 102, 2897.
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