$Three-dimensional brittle shear fracturing by tensile crack interaction$
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Three-dimensional brittle shear fracturing by tensile crack interaction

Faults in brittle rock are shear fractures formed through the interaction and coalescence of many tensile microcracks. The geometry of these microcracks and their surrounding elastic stress fields control the orientation of the final shear fracture surfaces. The classic Coulomb–Mohr failure criterio...

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Bibliographic Details
Main Authors:	Healy, David, Jones, R., Holdsworth, R.
Format:	Journal Article
Published:	Nature Publishing Group 2006
Online Access:	http://hdl.handle.net/20.500.11937/22462

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