On the similarity in the formation mechanism of the fracture structure of a rock massif

Local segments of the Earth’s crust reside at the mechanical nonequilibrium and continuously obtain and dissipate mechanical energy. The energy exchange between the structural elements of a geophysical medium determines its state, especially if the medium is fragmented into blocks. The stationary st...

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Veröffentlicht in:	Izvestiya. Physics of the solid earth 2011-04, Vol.47 (4), p.345-353
Hauptverfasser:	Bagdasar’yan, A. G., Sytenkov, V. N., Fedyanina, L. T., Shemetov, P. A.
Format:	Artikel
Sprache:	eng
Schlagworte:	Deformation Earth and Environmental Science Earth Sciences Energy conservation Energy dissipation Fractures Geophysics Geophysics/Geodesy Rocks Strain rate
Online-Zugang:	Volltext
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