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The structure of velocity mantle number of horizons under Phennoscandia according to seismic-tomography data
Seismic boundaries of the second kind have been distinguished under Phennoscandia according to three-dimensional P-velocity model of the mantle and velocity number of horizons of the upper mantle and its transitional zone has been shown. Four velocity horizons and corresponding seismic boundaries of...
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| Main Authors: | , |
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| Format: | Article |
| Language: | rus |
| Published: |
Subbotin Institute of Geophysics of the NAS of Ukraine
2016
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| Subjects: | |
| Online Access: | https://journals.uran.ua/geofizicheskiy/article/view/107723 |
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