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

dc.contributor.author	Gintov O.B.
dc.contributor.author	Murovskaya A.V.
dc.date.accessioned	2021-03-02T07:41:51Z
dc.date.available	2021-03-02T07:41:51Z
dc.date.issued	2001
dc.identifier	https://elibrary.ru/item.asp?id=27761607
dc.identifier.citation	Geophysical Journal, 2001, 20, 2, 213-243
dc.identifier.issn	0275-9128
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/26016
dc.description.abstract	The 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.subject	Cenozoic
dc.subject	Mesozoic
dc.subject	earth's crust
dc.subject	Crimean peninsula
dc.title	DYNAMICS OF THE EARTH'S CRUST OF THE CRIMEAN PENINSULA IN THE MESOZOIC-CENOZOIC (A TECTONOPHYSICAL ASPECT). PART 1
dc.type	Статья
dc.subject.age	Кайнозой	ru
dc.subject.age	Мезозой	ru
dc.subject.age	Cenozoic	en
dc.subject.age	Mesozoic	en

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