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...
Saved in:
| Date: | 2016 |
|---|---|
| Main Authors: | , |
| Format: | Article |
| Language: | Russian |
| Published: |
S. Subbotin Institute of Geophysics of the NAS of Ukraine
2016
|
| Subjects: | |
| Online Access: | https://journals.uran.ua/geofizicheskiy/article/view/107723 |
| Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
| Journal Title: | Geofizicheskiy Zhurnal |
Institution
Geofizicheskiy ZhurnalBe the first to leave a comment!