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...
| الحاوية / القاعدة: | Геофизический журнал |
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| المؤلفون الرئيسيون: | , |
| التنسيق: | مقال |
| اللغة: | الإنجليزية |
| منشور في: |
Subbotin Institute of Geophysics of the National Academy of Sciences of Ukraine
2016-02-01
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| الموضوعات: | |
| الوصول للمادة أونلاين: | https://journals.uran.ua/geofizicheskiy/article/view/107723 |