DYNAMICS OF A DESCENDING LITHOSPHERIC SLAB AND TECTONIC STRESSES IN CONTINENTAL COLLISION ZONES

dc.contributor.author	Ismail-Zadeh A.T.
dc.date.accessioned	2022-07-18T05:29:15Z
dc.date.available	2022-07-18T05:29:15Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=13452076
dc.identifier.citation	Doklady Earth Sciences, 2004, 395, 2, 296-298
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/38245
dc.description.abstract	A possible explanation of variations in the spatial localization of stresses and earthquakes related to them is given. It is assumed that the pressure gradient between the bottom and upper surface, tensile stresses and gravitation are the basic factors, governing a motion of merging plate. Analytical solution of problem on tensile mantle flows is suggested and possible reasons of changing in stressed state of mantle in the regions of continental collision are given. A model of two-dimensional flow of mantle is considered.
dc.title	DYNAMICS OF A DESCENDING LITHOSPHERIC SLAB AND TECTONIC STRESSES IN CONTINENTAL COLLISION ZONES
dc.type	Статья

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