@article{rosakis2002,
	Abstract = {Recent experimental observations of intersonic shear
rupture events that occur in a
variety of material systems have rekindled interest in the intersonic
failure phenomenon. Since the
early 1990s, engineers and scientists working in all length scales, from
the atomistic, the
structural, all the way up to the scale of the earth's deformation
processes, have undertaken joint
efforts to study this unexplored area of fracture mechanics. The
analysis in the present article
emphasizes the cooperative and complementary manner in which
experimental observations and
analytical and numerical developments have proceeded. The article first
reviews early contributions
to the theoretical literature of dynamic subsonic and intersonic
fracture and highlights the
significant differences between tensile and shear cracks. The article
then uses direct laboratory
observations as a framework for discussing the physics of intersonic
shear rupture occurring in
constitutively homogeneous (isotropic and anisotropic) as well as in
inhomogeneous systems, all
containing preferable crack paths or faults. Experiments, models, and
field evidence at a variety of
length scales (from the atomistic, the continuum, and up to the scale of
geological ruptures) are
used to discuss processes such as (1) shock wave formation, (2)
large-scale frictional contact and
sliding at the rupture faces, and (3) maximum attainable rupture speeds
and rupture speed stability.
Particular emphasis is given to geophysical field evidence and to the
exploration of the possibility
of intersonic fault rupture during shallow crustal earthquake events.},
	Author = {Rosakis, A. J.},
	Issue = {4},
	Journal = {Adv. Phys.},
	Month = {Jun},
	Pages = {1189--1257},
	Title = {Intersonic shear cracks and fault ruptures},
	Volume = {51},
	Year = {2002},
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The analysis in the present article emphasizes the cooperative and complementary manner in which experimental observations and analytical and numerical developments have proceeded. The article first reviews early contributions to the theoretical literature of dynamic subsonic and intersonic fracture and highlights the significant differences between tensile and shear cracks. The article then uses direct laboratory observations as a framework for discussing the physics of intersonic shear rupture occurring in constitutively homogeneous (isotropic and anisotropic) as well as in inhomogeneous systems, all containing preferable crack paths or faults. Experiments, models, and field evidence at a variety of length scales (from the atomistic, the continuum, and up to the scale of geological ruptures) are used to discuss processes such as (1) shock wave formation, (2) large-scale frictional contact and sliding at the rupture faces, and (3) maximum attainable rupture speeds and rupture speed stability. Particular emphasis is given to geophysical field evidence and to the exploration of the possibility of intersonic fault rupture during shallow crustal earthquake events.","author":[{"propositions":[],"lastnames":["Rosakis"],"firstnames":["A.","J."],"suffixes":[]}],"issue":"4","journal":"Adv. 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Since the\nearly 1990s, engineers and scientists working in all length scales, from\nthe atomistic, the\nstructural, all the way up to the scale of the earth's deformation\nprocesses, have undertaken joint\nefforts to study this unexplored area of fracture mechanics. The\nanalysis in the present article\nemphasizes the cooperative and complementary manner in which\nexperimental observations and\nanalytical and numerical developments have proceeded. The article first\nreviews early contributions\nto the theoretical literature of dynamic subsonic and intersonic\nfracture and highlights the\nsignificant differences between tensile and shear cracks. The article\nthen uses direct laboratory\nobservations as a framework for discussing the physics of intersonic\nshear rupture occurring in\nconstitutively homogeneous (isotropic and anisotropic) as well as in\ninhomogeneous systems, all\ncontaining preferable crack paths or faults. Experiments, models, and\nfield evidence at a variety of\nlength scales (from the atomistic, the continuum, and up to the scale of\ngeological ruptures) are\nused to discuss processes such as (1) shock wave formation, (2)\nlarge-scale frictional contact and\nsliding at the rupture faces, and (3) maximum attainable rupture speeds\nand rupture speed stability.\nParticular emphasis is given to geophysical field evidence and to the\nexploration of the possibility\nof intersonic fault rupture during shallow crustal earthquake events.},\n\tAuthor = {Rosakis, A. J.},\n\tIssue = {4},\n\tJournal = {Adv. 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