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

E. Kozlovskaya
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, even these rare studies showed that the upper mantle there is heterogeneous and seismically anisotropic. In order improve this knowledge, a temporary seismic array was installed in May 2007, and operated...
6 citations reported since publication in 2007.
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