Seismic network XK:LAPNET/POLENET seismic temporary array (RESIF-SISMOB)

Deep structure of the crust and upper mantle of the northern, mainly Archaean part of the Fennoscandian shield, is poorly known, as the number of permanent seismic stations and controlled-source seismic profiles there has been always significantly lower compared to its southwestern part. However, ev...

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Bibliographic Details
Main Author: Kozlovskaya, E.
Format: Article in Journal/Newspaper
Language:English
Published: RESIF - Réseau Sismologique et géodésique Français 2007
Subjects:
Dun
IPY
Online Access:https://dx.doi.org/10.15778/resif.xk2007
https://seismology.resif.fr/networks/#/XK__2007