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 o...
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| Hlavní autoři: | , |
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| Médium: | Artigo |
| Jazyk: | Inglês |
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Subbotin Institute of Geophysics of the National Academy of Sciences of Ukraine
2016-02-01
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| Edice: | Геофизический журнал |
| Témata: | |
| On-line přístup: | https://journals.uran.ua/geofizicheskiy/article/view/107723 |
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