DYNAMICS OF THE EARTH'S CRUST OF THE CRIMEAN PENINSULA IN THE MESOZOIC-CENOZOIC (A TECTONOPHYSICAL ASPECT). PART 2

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 deformation stages of Mesozoic-Cenozoic deposits in the Crimean Peninsula were identified on the basis of structural-paragenetic and kinematic analyses of cracks and glide planes. The Late-Jurassic age of the Karadag volcanic massif was confirmed. It seems that the Upper-Jurassic rocks occur virtually autochthonously. Variation of the relationship between the main stresses during deformation was studied. A tectonophysical model of the dynamic system of the Southern-coast seismic zone is discussed.
dc.identifierhttps://elibrary.ru/item.asp?id=27761746
dc.identifier.citationGeophysical Journal, 2001, 20, 3, 425-446
dc.identifier.issn0275-9128
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/26018
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 2
dc.typeСтатья

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