GENERAL MECHANISM OF FOLDING

dc.contributor.author	Kuliyev G.G.
dc.contributor.author	Buryakovskiy L.A.
dc.contributor.author	Dzhevanshir R.D.
dc.date.accessioned	2020-10-06T05:10:44Z
dc.date.available	2020-10-06T05:10:44Z
dc.date.issued	1989
dc.identifier	https://elibrary.ru/item.asp?id=31091012
dc.identifier.citation	Transactions (Doklady) of the USSR Academy of Sciences. Earth Science Sections, 1989, , 2, 80-82
dc.identifier.issn	0891-5571
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/17754
dc.description.abstract	In this paper we present a mathematical model of a general mechanism of folding. We emphasize that in this formulation the nature of the forces producing the folding is immaterial. The rather general character of the model enables us to give these forces and other parameters specific geometric, mechanical, or mining geological interpretations of various kinds and to make a qualitative and quantitative analysis of the concrete results. Our approach uses the three-dimensional linearized theory of stability and differs from the earlier studies, which investigate stability only in the case of uniaxial compression, by taking fuller and more diverse account of the factors that produce loss of stability and of the boundary conditions (which are fundamental in stability problems) accompanying this process.
dc.title	GENERAL MECHANISM OF FOLDING
dc.type	Статья

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