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Published in 2020 at "Tectonophysics"
DOI: 10.1016/j.tecto.2020.228574
Abstract: Abstract The northern part of the Fennoscandian shield records several Palaeoproterozoic phases of rifting, crustal shortening, metamorphism and structural reactivation. The geologic history has left behind a complex crustal geoelectric structure as evidenced by magnetotelluric…
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Keywords:
central lapland;
finnish lapland;
lapland;
phase tensor ... See more keywords