RELATIONSHIPS BETWEEN THE KINEAMATICS OF THE TOP OF A LAYER AND THE STATE OF STRESS WITHIN IT DUE TO BLOCK MOTION AT ITS BOTTOM (IN CONNECTION WITH THE INTERPRETATION OF RECENT MOVEMENTS)

dc.contributor.author	Mikhailova A.V.
dc.contributor.author	Rebetsky Y.L.
dc.contributor.author	Grigoryev A.S.
dc.contributor.author	Volovich I.M.
dc.contributor.author	Shakhmuradova Z.E.
dc.date.accessioned	2020-04-16T07:05:59Z
dc.date.available	2020-04-16T07:05:59Z
dc.date.issued	1988
dc.identifier	https://elibrary.ru/item.asp?id=31009901
dc.identifier.citation	JOURNAL OF GEODYNAMICS, 1988, 10, 2-4, 127-138
dc.identifier.issn	0264-3707
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/16850
dc.description.abstract	The equilibrium of an infinite linearly viscous layer overlying a rigid basement which is separated into blocks by a narrow plane slit is considered. The state of stress in the layer is caused by slow translational motions of the basement blocks. This spatial problem is shown to separate into problems of plane and anti-plane strain; their solutions are constructed in analytic form. The theoretical study was accompanied by modelling experiments. The results are applied to a kinematic interpretation of recent movements in sediments.
dc.title	RELATIONSHIPS BETWEEN THE KINEAMATICS OF THE TOP OF A LAYER AND THE STATE OF STRESS WITHIN IT DUE TO BLOCK MOTION AT ITS BOTTOM (IN CONNECTION WITH THE INTERPRETATION OF RECENT MOVEMENTS)
dc.type	Статья

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