DYNAMICS OF THE EARTH'S CRUST OF THE CRIMEAN PENINSULA IN THE MESOZOIC-CENOZOIC (A TECTONOPHYSICAL ASPECT). PART 1

dc.contributor.authorGintov O.B.
dc.contributor.authorMurovskaya A.V.
dc.date.accessioned2021-03-02T07:41:51Z
dc.date.available2021-03-02T07:41:51Z
dc.date.issued2001
dc.description.abstractThe main stages of deformation of Meso-Cenozoic age of the Crimean peninsula were identified on the basis of structure-parageneses and kinematic analyses of cracks and glide planes. The Late-Jurassic age of the Karadag volcanic massif was proven. It seems that the Late-Jurassic rocks occured mainly autochthonously. Variation of the relationship between the principal normal stresses in the course of deformation was established. A tectonophysical model of the dynamic system of the southern-shore seismic zone was developed.
dc.identifierhttps://elibrary.ru/item.asp?id=27761607
dc.identifier.citationGeophysical Journal, 2001, 20, 2, 213-243
dc.identifier.issn0275-9128
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/26016
dc.subjectCenozoic
dc.subjectMesozoic
dc.subjectearth's crust
dc.subjectCrimean peninsula
dc.subject.ageMesozoicen
dc.titleDYNAMICS OF THE EARTH'S CRUST OF THE CRIMEAN PENINSULA IN THE MESOZOIC-CENOZOIC (A TECTONOPHYSICAL ASPECT). PART 1
dc.typeСтатья

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