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J-GLOBAL ID:200902083255296579   Reference number:87A0415800

Anisotropic development of dilatancy in uniaxially compressed granites.

花こう岩のダイレイタンシー異方性について
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Issue: 382  Page: 63-72  Publication year: Jun. 1987 
JST Material Number: F0028A  ISSN: 0289-7806  Document type: Article
Article type: 原著論文  Country of issue: Japan (JPN)  Language: JAPANESE (JA)
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Mechanical properties of rocks 
Reference (16):
  • 1) Brace, W. F., Paulding, B. W. and Scholz, C. H.: Dilatancy in the fracture of crystalline rocks, J. Geophys. Res., Vol. 71, pp. 3939-3953, 1966.
  • 2) Scholz, C. H.: Microfracturing and the inelastic deformation of rock in compression, J. Geophys. Res., Vol. 73, pp. 1417-1432, 1968.
  • 3) Kranz, R. L.: Crack-crack and crack-pore interactions in stressed granite, Int. J. Rock Mech. Min. Sci. & Geomech. Abstr., Vol. 16, pp. 37-47, 1979.
  • 4) Spetzler, H.: Seismic velocity changes during fracture and frictional sliding, Pure Appl. Geophys., Vol. 116, pp. 732-742, 1978.
  • 5) Yanagidani, T., Ehara, S., Nishizawa, O., Kusunose, K. and Terada, M.: Localization of dilatancy in Ohshima granite under constant uniaxial stress, J. Geophys. Res., Vol. 90, pp. 6840-6858, 1985.
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