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Paleozoic exotic blocks of the crimean mountains: stratigraphy and origin

dc.contributor.authorYutsis, Vsevolod
dc.contributor.authorTatiana Sukhanova
dc.contributor.editorScientific Research Publishing Inc
dc.date.accessioned2018-03-22T23:17:38Z
dc.date.available2018-03-22T23:17:38Z
dc.date.issued2014-08
dc.identifier.citationYutsis, V. , Stafeev, A. and Sukhanova, T. (2014) Paleozoic Exotic Blocks of the Crimean Mountains: Stratigraphy and Origin. Open Journal of Geology, 4, 364-372. doi: 10.4236/ojg.2014.48028.
dc.identifier.urihttp://hdl.handle.net/11627/3573
dc.description.abstract"Based on numerous geological data obtained by the authors for several decades, the stratification of Permian and Carboniferous ancient and exotic blocks of Crimean Mountains is performed. The sequence of geological events that cause their origin is revealed. Carnian-Norian, Rhaetian-Hettangian and Early-Pliensbachian phases of collapse, sliding and burial of Paleozoic blocks are specified. Final stage (block re-deposition) is confined to the Toarcian and Aalenian ages. The data obtained allow re-interpreting the origin of ancient exotic blocks of the Crimea."
dc.rightsAttribution-NonCommercial-NoDerivatives 4.0 Internacional
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/
dc.subjectCrimea
dc.subjectPaleozoic Blocks
dc.subjectPaleogeography
dc.subjectStratigraphy
dc.subject.classificationGEOLOGÍA
dc.titlePaleozoic exotic blocks of the crimean mountains: stratigraphy and origin
dc.typearticle
dc.identifier.doihttp://dx.doi.org/10.4236/ojg.2014.48028
dc.rights.accessAcceso Abierto


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Attribution-NonCommercial-NoDerivatives 4.0 Internacional
Except where otherwise noted, this item's license is described as Attribution-NonCommercial-NoDerivatives 4.0 Internacional