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On the nature of the anomalies of the velocity of propagation of longitudinal seismic waves in the upper mantle
P-velocity models of the upper mantle for the regions with different endogenous regimes on the continents and oceans (Precambrian platforms, zones of young activization, Alpine geosynclines, rifts, deep basins, mid-ocean ridges, margin trenches) have been considered. Thermal models and standard comp...
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Format: | Article |
Language: | rus |
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Subbotin Institute of Geophysics of the NAS of Ukraine
2010
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Online Access: | https://journals.uran.ua/geofizicheskiy/article/view/117556 |
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