Browsing ELibrary by Author "Kaban M.K."
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Browsing ELibrary by Author "Kaban M.K."
Now showing items 1-10 of 10
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Kaban M.K. (2004)This work continues a series of papers investigating the density structure of the North Eurasian lithosphere. Based on the 3-D density model of the lithosphere, which was constructed at the preceding stage of the investigations, ...
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Kaban M.K. (2001)A numerical density model of the North Eurasia crust is constructed and its gravity effect is calculated. This model includes variations in the thickness and density of the sedimentary cover and solid crust, derived from ...
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Kaban M.K. (2002)A density model of the lithosphere for the Caucasus, Kopet-Dagh, a part of Tien-Shan, Caspian and Black seas, as well as for adjacent parts of East European platform and Turanian plate is constructed based on an integrated ...
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Kaban M.K.; Schwintzer P.; Artemieva I.M.; Mooney W.D. (2003)The origin and evolution of cratonic roots has been debated for many years. Precambrian cratons are underlain by cold lithospheric roots that are chemically depleted. Thermal and petrologic data indicate that Archean roots ...
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Grachev A.F.; Kaban M.K.; Nikolaev V.A. (2004)
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Artemev M.E.; Belov A.P.; Kaban M.K.; Karaev A.I. (1992)
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Artemjev M.E.; Kaban M.K. (1991)At present, there are two concepts of the term isostasy. According to the first one, isotasy means hydrostatic pressure conditions at the depth of compensation existing due to mass distributions above that depth. The second ...
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Kaban M.K.; Schwintzer P. (2001)Isotropic shear-wave velocities from the Ekström/Dziewonski S20 global tomographic model and residual `crust-free' gravity are used to determine density-velocity relations for various mantle layers by inversion. The residual ...
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Vinnik L.P.; Aleshin I.M.; Kosarev G.L.; Oreshin S.I.; Reigber C.; Kaban M.K.; Roecker S.W. (2004)To obtain an image of the deep structure of the Tien Shan in central Asia, we invert P and S receiver functions jointly for almost 40 local broad-band seismograph stations. The inversion is performed using a simulated ...
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Kaban M.K.; Artemjev M.E. (1986)If crustal material (including water in oceanic areas) is compressed to the mean density of the subcrustal layer, the surface of the body can be considered as a free mantle surface (FM)). Joint analysis of FMS and of gravity ...
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