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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Format: | Article in Journal/Newspaper |
Language: | English |
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RESIF - Réseau Sismologique et géodésique Français
2007
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Online Access: | https://dx.doi.org/10.15778/resif.xk2007 https://seismology.resif.fr/networks/#/XK__2007 |