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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| Date: | 2016 |
|---|---|
| Main Authors: | Tsvetkova, T. A., Bugaenko, I. V. |
| Format: | Article |
| Language: | Russian |
| Published: |
S. 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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| Journal Title: | Geofizicheskiy Zhurnal |
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