Zobrazeno 1 - 10 of 13 pro vyhledávání: '"E. V. Artyushkov"'
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Akademický článek
Accelerated non-linear destruction of the earth's crust
Autor: E. V. Artyushkov
Publikováno v: Discrete Dynamics in Nature and Society, Vol 6, Iss 4, Pp 281-290 (2001)
The upper part of the Earth—the lithospheric layer, ∼100 km thick, is rigid. Segments of this spherical shell–lithospheric plates are drifting over a ductile asthenosphere. On the continents, the lithosphere includes the Earth's crust, ∼40 km
Externí odkaz: https://doaj.org/article/5486cf12ee254208a1d71d7a70b06dd1
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5
Vertical crustal movements on the continents as a reflection of deep-seated processes in the earth’s crust and mantle: Geological effects
Autor: E. V. Artyushkov
Publikováno v: Herald of the Russian Academy of Sciences. 82:432-446
The large volume of studies conducted makes it possible to assert that the recent geological history of the earth is characterized by rapid vertical crustal movements, which resulted in the formation of vast elevated areas and deep depressions. The e
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::eb035bb9671a33c80d40a63659f2ee3a
https://doi.org/10.1134/s101933161206007x
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6
On the Isostatic Equilibrium of the Earth's Crust
Autor: E. V. Artyushkov
Publikováno v: Geophysical Journal of the Royal Astronomical Society. 14:251-260
Summary A brief physical analysis of the postglacial uplift of Fennoscandia is presented. It permits one to detect the great decrease in viscosity in a relatively thin layer of the upper mantle substance. The existence of this layer, i. e. the asthen
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::c71469a0c63c2a38cee420c9b3ff8af1
https://doi.org/10.1111/j.1365-246x.1967.tb06242.x
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9
On the mechanism of formation of the tyrrhenian sea
Autor: E. V. Artyushkov, Enzo Boschi, S. Zerbini
Publikováno v: Pure and Applied Geophysics PAGEOPH. 121:39-62
We investigated some of the existing hypotheses on the formation of the Tyrrhenian Sea basin, and we found that none of them appears satisfactory. By quantitative considerations we show that proposed mechanisms, such as those based on oceanization or
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::30a149be9e2f34d3b22116737eca2e5c
https://doi.org/10.1007/bf02590119
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10
Rheological properties of the crust and upper mantle according to data on isostatic movements
Autor: E. V. Artyushkov
Publikováno v: Journal of Geophysical Research. 76:1376-1390
A physical analysis of the isostatic movements in Canada, in West Siberia, and in the region of Pleistocene Lake Bonneville in the Rocky Mountains is given. It is shown that the low-viscosity (of the order of 1020 poises) layer exists beneath the Can
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::8f84c515b0467393fc98c36e05988004
https://doi.org/10.1029/jb076i005p01376
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