HIERARCHICAL PROPERTIES OF A STRESS FIELD AND ITS RELATION TO FAULT DISPLACEMENTS

dc.contributor.author	Osokina D.N.
dc.date.accessioned	2020-04-08T04:42:09Z
dc.date.available	2020-04-08T04:42:09Z
dc.date.issued	1988
dc.identifier	https://elibrary.ru/item.asp?id=30891630
dc.identifier.citation	JOURNAL OF GEODYNAMICS, 1988, 10, 2-4, 331-344
dc.identifier.issn	0264-3707
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/16363
dc.description.abstract	The structure of the stress field is studied around a frictional shear fault on the basis of a theoretical solution. The hierarchical properties of tectonic stress fields are discussed. A method is proposed for the separation of fields of different ranks. It is shown that displacements of sides are dependent on the fault-plane orientation in the initial stress field and the type of that field; and on the coefficient of friction. These displacements are the greatest on planes that make angles below 45° with the compression axis of the initial field.
dc.title	HIERARCHICAL PROPERTIES OF A STRESS FIELD AND ITS RELATION TO FAULT DISPLACEMENTS
dc.type	Статья

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