DYNAMICS OF A DESCENDING LITHOSPHERIC SLAB AND TECTONIC STRESSES IN CONTINENTAL COLLISION ZONES
- DSpace Home
- →
- Геология России
- →
- ELibrary
- →
- View Item
JavaScript is disabled for your browser. Some features of this site may not work without it.
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 |
Files in this item
Files | Size | Format | View |
---|---|---|---|
There are no files associated with this item. |
This item appears in the following Collection(s)
-
ELibrary
Метаданные публикаций с сайта https://www.elibrary.ru