BENDING STIFFNESS OF THE LITHOSPHERE OF EURASIA

dc.contributor.author	Kukuliyeva R.Y.
dc.contributor.author	Kogan M.G.
dc.date.accessioned	2020-04-08T08:53:50Z
dc.date.available	2020-04-08T08:53:50Z
dc.date.issued	1988
dc.identifier	https://elibrary.ru/item.asp?id=30934531
dc.identifier.citation	TRANSACTIONS (DOKLADY) OF THE USSR ACADEMY OF SCIENCES. EARTH SCIENCE SECTIONS, 1988, 301, 4, 8-12
dc.identifier.issn	0891-5571
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/16407
dc.description.abstract	The authors used the gravitational admittance technique in an investigation of the isostasy of the Urals, in which they also employed an analysis of the coherence between topography and the gravity anomalies, plus a semiquantitative analysis of the length of the foredeep. Mutually consistent estimates of the thickness of the lithosphere were obtained. Three different approaches, i.e., gravitational admittance, the length of the foredeep, and analysis of the coherence between gravitational anomalies and topography give the following mutually consistent results: (1) the strong cold lithosphere of the Russian plate supports the Urals; (2) the gravitational anomalies of the Urals zone are governed both by topography and by high density loads at depth; (3) analysis of the coherence between gravitational anomalies and topography is an effective method of investigating isostasy in continental regions.
dc.title	BENDING STIFFNESS OF THE LITHOSPHERE OF EURASIA
dc.type	Статья

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