Supersonic and intersonic cracking in rock-like material under remote stresses. Sibiriakov, B. P. Theor. Appl. Fract. Mec., 38:255--265, Nov, 2002.
abstract   bibtex   
There are many models that attempt to describe the dynamics of seismology that include plasticity, temperature effect, dissipation and viscosity. While these details are important, useful results of dynamic deformation can be obtained from simple models. The essential features are the internal geometry of porosity and cracked medium. They involve the specific surface or the average distance between one crack to another. This entails the internal sizes of micro and mesostructure that are not considered by classical mechanics. Only one new parameter is introduced in the simple model, the specific surface while the other parameters are the Lame constants and density. (C) 2002 Elsevier Science Ltd. All rights reserved.
@article{sibiriakov2002,
	Abstract = {There are many models that attempt to describe the
dynamics of seismology that
include plasticity, temperature effect, dissipation and viscosity. While
these details are
important, useful results of dynamic deformation can be obtained from
simple models. The essential
features are the internal geometry of porosity and cracked medium. They
involve the specific surface
or the average distance between one crack to another. This entails the
internal sizes of micro and
mesostructure that are not considered by classical mechanics. Only one
new parameter is introduced
in the simple model, the specific surface while the other parameters are
the Lame constants and
density. (C) 2002 Elsevier Science Ltd. All rights reserved.},
	Author = {Sibiriakov, B. P.},
	Date-Modified = {2010-07-14 12:41:30 -0700},
	Issue = {3},
	Journal = {Theor. Appl. Fract. Mec.},
	Month = {Nov},
	Pages = {255--265},
	Title = {Supersonic and intersonic cracking in rock-like material under remote stresses},
	Volume = {38},
	Year = {2002},
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