THE STRUCTURAL ARCHITECTURE OF THE FOOTWALL TO THE MAIN URALIAN FAULT, SOUTHERN URALS
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dc.contributor.author | Brown D. | |
dc.contributor.author | Alvarez-Marron J. | |
dc.contributor.author | Perez-Estaun A. | |
dc.contributor.author | Puchkov V. | |
dc.date.accessioned | 2020-11-30T07:39:34Z | |
dc.date.available | 2020-11-30T07:39:34Z | |
dc.date.issued | 1996 | |
dc.identifier | https://elibrary.ru/item.asp?id=13229156 | |
dc.identifier.citation | Earth-Science Reviews, 1996, , 1, 125-147 | |
dc.identifier.issn | 0012-8252 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/19935 | |
dc.description.abstract | The Uralide orogen is a linear collisional belt formed during the Upper Paleozoic as a result of convergence between the East European Craton and outboard terranes, and accretion of intervening island arcs and obduction of oceanic crust onto the East European Craton. This paper presents a new structural subdivision of the southern Urals, to the west of the main suture zone, that puts this part of the mountain belt in a context similar to that of other collisional orogenic belts. This subdivision consists of a west-vergent thrust stack that is made up of an autochthonous to parautochthonous foreland basin, and a parautochthonous foreland thrust and fold belt, flanked to the east by a metamorphic thrust stack. The latter units are structurally overlain by allochthonous rocks of an accretionary complex, slope sediments, oceanic crust and high grade, eclogite-blueschist-bearing, gneiss. Where possible these units are defined on the basis of their internal stratigraphy and structure and on the nature of their bounding faults. | |
dc.subject | Paleozoic | en |
dc.title | THE STRUCTURAL ARCHITECTURE OF THE FOOTWALL TO THE MAIN URALIAN FAULT, SOUTHERN URALS | |
dc.type | Статья | |
dc.subject.age | Paleozoic | en |
dc.subject.age | Палеозой | ru |
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