TO PROBLEM OF DEFORMED BODY DESTRUCTION. PART 1. THE MAIN EQUATIONS

dc.contributor.author	Chanyshev A.I.
dc.date.accessioned	2021-03-20T04:39:35Z
dc.date.available	2021-03-20T04:39:35Z
dc.date.issued	2001
dc.identifier	https://www.elibrary.ru/item.asp?id=14957434
dc.identifier.citation	Fiziko-Texhnicheskiye Problemy Razrabbotki Poleznykh Iskopaemykh, 2001, , 3, 53-67
dc.identifier.issn	0015-3273
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/26972
dc.description.abstract	Phenomenon of deformed rock mass destruction has been considered. Mathematical models of rock mass destruction have been discussed. It has been shown that system of differential equations of hyperbolic type describes rock mass destruction in case of plane deformation. Relation between hydrostatic stress and maximal tangential stress is described by means of four orthogonal characteristics. Turn of rocks and value of angle characterizing the positions of the main axes of stress tensor have been shown. In order to determine various parameters on boundary of region, Cauchy stress vectors and displacements are preset.
dc.title	TO PROBLEM OF DEFORMED BODY DESTRUCTION. PART 1. THE MAIN EQUATIONS
dc.type	Статья

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