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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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Bibliographic Details
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
Subjects:	seismic tomography seismic boundaries of the second kind
Online Access:	https://journals.uran.ua/geofizicheskiy/article/view/107723
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Journal Title:	Geofizicheskiy Zhurnal

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Geofizicheskiy Zhurnal

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